Article

The Formation Models of Gypsum Barrier, Chemical Temporal Changes and Assessments the Water Quality of Sawa Lake, Southern Iraq

Authors:
  • University of Baghdad - College of Scinece
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Abstract

This study deals with formation models of gypsum barrier, chemical temporal changes, and assessments of the Sawa Lake within the Al- Muthanna province, Southern Iraq, it is a very important issue to find the water quality and water assessments of this lake. Eleven water samples are collected from Sawa Lake. Many scientific concepts are used such as major cations (Ca2+, Mg2+, Na+ and K+), major anions (SO4=,Cl-,HCO3- and CO3=) with minor anions ( PO43-, NO3-) and H2S . Trace elements (Pb, Cd, Zn, As, Ni, Co, Cu, Mn, Fe, As, Sr And B) and bacterial test were analyzed in each sample. Total dissolved solids (TDS), electrical conductivity (EC), pH and temperature (T) were directly measured in the field. The equilibrium state between the concentration and evaporation contributed actively to build the salt wall surrounded the lake. The building wall of the Lake is a barrier of gypsum, which is in a dynamic state between construction and dissolution.The length of gypsum barrier surrounding the lake is 12.5 km with 3-6 m high. Gypsum wall collapse occurs in abundance in the sites that face the wind which activates the erosion processes. The chemistry of Sawa Lake during 1977, 1983 and 2003 was Na- SO4=; then it was changed to be as Mg-Cl from during 2007and 2011 (present study). This study revealed that theSawa Lake water is as unsuitable for drinking, livestock and irrigationpurposes.

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... The geological effects governed the creation of Sawa Lake in the region about (10,000) years ago [91,92]. Tectonically, the lake is situated as a part of the western desert, at the boundary between the stable shelf (Salman subzone) and the unstable shelf ...
... Sawa Lake is supplied with water mainly by groundwater merge between the deep and shallow aquifers beneath the lake; especially the Euphrates, Dammam, and Er Radhuma through a system of joints and cracks [93]. It is believed that Sawa Lake is of marine origin water due to the mixing of Dammam Formation water (meteoric and rich with CaSo 4 ) with Euphrates Formation water (marine origin) [92]. The hydrogeochemical index (Cl/HCO 3 ) of the lake water is very high compared to inland water and close to that of seawater which reflect the effect of seawater. ...
... The geological formations beneath the lake are aquifers such as ErRadhuma, Dammam, and Euphrates Formations. The recharge areas of the aquifers that beneath the lake are from adjacent highlands and the piezometric pressure raises the water upward to fill the lake depression[92]. ...
Thesis
Full-text available
In the present study, seasonal measurements of radon activity concentration were carried out for water and soil of Sawa Lake, Samawa City-South of Iraq. The measurements were conducted in two seasons, winter and spring, using RAD7 continuous radon monitoring detector manufactured by Durridge company, USA. For winter season, (85) water samples were collected from different locations; the period of assessment was two months (from December, 1st 2018 to February, 1st 2019). Radon activity concentrations were ranged from (0.085 Bq/L) to (0.965 Bq/L), while the average value was (0.322 Bq/L), the annual effective dose (AED) of inhalation was estimated and is found to be ranged from (0.000080 mSv.y-1) to (0.000917 mSv.y-1) with a mean value of (0.000325 mSv/y). Radon measurements during the spring season have been carried out with a period of two months (from March 1st, 2019, to April 26, 2019). Radon concentrations have been determined for (85) collected water samples and found to be in the range of (0.093±0.085 Bq/L) and (1.15±0.35 Bq/L) with an average value of (0.409±0.24 Bq/L), the annual inhalation dose in the spring season varied between (0.0000883 mSv/y) and (0.001065 mSv/y); with an average value of (0.000389 mSv/y). Physiochemical parameters such as pH, EC, TDS, resistivity, and turbidity were determined for the collected water samples during both seasons and the correlation between these parameters and radon concentrations was established. Radon concentrations in soil gas have been measured during winter and spring seasons. A total of (30) locations around the lake in each season were chosen for in situ analyzing. RAD7 detector is used for this purpose. Radon soil gas activity concentration for the winter season is found to vary from (86.9 ± 54 Bq/m3) and (6448 ±480 Bq/m3) with an average value of (1963±267 Bq/m3). Associated annual effective dose due to inhalation has been found to be in the range of (0.000826-0.061282 mSv/y), with an average value of (0.01866 mSv/y). For the spring season, radon concentrations in soil gas varied from (40 ±50 Bq/m3) to (4970±360 Bq/m3), with a mean value of (1434.17 ±205 Bq/m3). Annual inhalation dose due to these concentrations has been estimated and is found to vary between (0.000380 mSv/y) and (0.061282 mSv/y), with an average value of (0.01363 mSv/y).
... The evaporate lithofacies is the main mineralogical facies (Awadh and Muslim, 2014) in the lake, where it is represented by gypsum that forms an amount varies between 67.5% and 97.5% with average of 87% from the total lake sediment ( Table 1). The water body in the Sawa Lake is considered as a super-saturation solution that mainly contains calcium and sulfates. ...
... It feeds by groundwater at different levels via fractures, fissures and joints. The water level in the lake depends regionally on the recharged area, doesn't locally (Awadh and Muslim, 2014). The height of the wall surrounding the lake is about 6 m. ...
... Crystallization is active in the shallow sites that represent the boundary of the lake. Gypsum grows with time and rises upward to be higher than the water level; hence capillary process absorbs water upward to the surface of crystallized gypsum nuclei then evaporate under high temperature forming strange shapes of gypsum masses resembling cauliflower (Awadh and Muslim, 2014). Lake derives water from groundwater reservoir sets that are located underneath. ...
... The evaporate lithofacies is the main mineralogical facies (Awadh and Muslim, 2014) in the lake, where it is represented by gypsum that forms an amount varies between 67.5% and 97.5% with average of 87% from the total lake sediment ( Table 1). The water body in the Sawa Lake is considered as a super-saturation solution that mainly contains calcium and sulfates. ...
... It feeds by groundwater at different levels via fractures, fissures and joints. The water level in the lake depends regionally on the recharged area, doesn't locally (Awadh and Muslim, 2014). The height of the wall surrounding the lake is about 6 m. ...
... Crystallization is active in the shallow sites that represent the boundary of the lake. Gypsum grows with time and rises upward to be higher than the water level; hence capillary process absorbs water upward to the surface of crystallized gypsum nuclei then evaporate under high temperature forming strange shapes of gypsum masses resembling cauliflower (Awadh and Muslim, 2014). Lake derives water from groundwater reservoir sets that are located underneath. ...
Article
This work has been accomplished through a dense field work on the Sawa Lake. The aim of this work is to highlight on characteristics that are consistent with outstanding universal values to be a new Iraqi site belongs to the World Natural Heritage. This study sorted many unique characteristics might ensure that Sawa Lake as a world natural heritage sites. This study shows that the lake had met four natural criteria of the outstanding universal values: (1) the seventh criterion which states to contain superlative natural phenomena or areas of exceptional natural beauty and aesthetic importance. (2) The eighth criterion which stated to be outstanding example representing major stages of earth's history, including the record of life, significant on-going geological processes in the development of landforms, or significant geomorphic or physiographic features. (3) The ninth criterion which stated to be outstanding examples representing significant on-going ecological and biological processes in the evolution and development of terrestrial, fresh water, coastal and marine ecosystems and communities of plants and animals. (4) The tenth criterion which state to contain most important and significant natural habitats for in-situ conservation of biological diversity, including those containing threatened species of outstanding universal value from the point of view of science or conservation.
... The composition of groundwater is subject to the influence of many climatic factors, topography and hydrographic nature. However, the main effect on groundwater quality is through the chemical composition of the water-bearing rocks and the chemical composition of the deep water that participates in feeding the water-bearing levels located at the top and coming to it through the weak permeability separating layers [1]. Therefore, one of the most important objectives of this research is to study the hydrochemical situation prevailing in the study area, its physical and chemical properties. ...
... The acidic function ( pH) is the negative logarithm of the concentration of the hydrogen ion, and it is considered a measure of the acidity and basicity in normal temperature and pressure [10]. The highest value pH. was in Well No. (1). This reached (8.7), and the lowest value was in Wells No. (2) (7.1). ...
Article
Full-text available
Twenty-five groundwater samples from the Al-Zubair area, southern Iraq, were analyzed for physical and chemical variables. The study showed that the groundwater is of acidic type and in it tends towards light alkalinity. Both electrical conductivity and the total dissolved solids showed increased concentrations of sodium, calcium, magnesium, potassium and sulfate, chloride, bicarbonate, and nitrate. The hydrochemical formula for most groundwater wells are (Ca-Cl), (Ca-SO4), (Mg-SO4), and (Na-Cl) type due to the high concentrations of these ions in the water., it was found that this water is not suitable for human drinking. Due to its high salinity compared to the requirements of international standard and Iraqi standard standards, while it is suitable for drinking animal's construction purposes, it has not exceeded the permissible limits. Also, it has been found that this water is not suitable for industrial and irrigation purposes, where it is possible to grow crops that tolerate high salinity ‫ل‬ ‫بيئية‬ ‫اسة‬ ‫در‬ ‫نوعية‬ ‫الزبير‬ ‫في‬ ‫المختارة‬ ‫االبار‬ ‫بعض‬ ‫في‬ ‫الجوفية‬ ‫المياه‬ ، ‫جنوب‬ ‫ي‬ ‫استعماالتها‬ ‫و‬ 2 ‫جيجان‬ ‫بتول‬ ، 1 ‫االمير‬ ‫عبد‬ ‫فاطمة‬ ، *1 ‫الخفاجي‬ ‫رعد‬ ‫اق‬ ‫العر‬ ‫بغداد،‬ ‫بغداد،‬ ‫جامعة‬ ‫الهيثم)،‬ ‫فه(ابن‬ ‫الصر‬ ‫للعلوم‬ ‫بيه‬ ‫التر‬ ‫كلية‬ ، ‫الحياة‬ ‫علوم‬ ‫قسم‬ 1 2 ، ‫الحياة‬ ‫علوم‬ ‫قسم‬ ‫ثانوية‬ ‫كلية‬ ‫بغداد،‬ ‫اق‬ ‫العر‬ ‫بغداد،‬ ‫الخالصة‬ ‫تم‬ ‫اختيار‬ 25 ‫اق‬ ‫العر‬ ‫جنوب‬ ‫بير‬ ‫الز‬ ‫منطقة‬ ‫من‬ ‫ة‬ ‫مختار‬ ‫ألبار‬ ‫الجوفية‬ ‫المياه‬ ‫من‬ ‫عينة‬ ‫المياه‬ ‫نوعية‬ ‫فة‬ ‫لمعر‬ ‫حيث‬ ‫حمضية‬ ‫اسة‬ ‫الدر‬ ‫منطقة‬ ‫في‬ ‫الجوفية‬ ‫المياه‬ ‫أن‬ ‫النتائج‬ ‫أظهرت‬ ‫الكيميائية.‬ ‫و‬ ‫يائية‬ ‫الفيز‬ ‫ات‬ ‫المتغير‬ ‫تحديد‬ ‫خالل‬ ‫بعض‬ ‫في‬ ‫الذائبة‬ ‫الصلبة‬ ‫اد‬ ‫المو‬ ‫و‬ ‫بائية‬ ‫الكهر‬ ‫التوصيلية‬ ‫من‬ ‫كال‬ ‫تركيز‬ ‫في‬ ‫يادة‬ ‫ز‬ ‫هناك‬ ‫الخفيفة.‬ ‫القلوية‬ ‫نحو‬ ‫تميل‬ ‫اس‬ ‫در‬ ‫اظهرت‬ ‫االبار.‬ ‫تلك‬ ‫مياه‬ ‫يد‬ ‫الكلور‬ ‫و‬ ‫يتات‬ ‫الكبر‬ ‫و‬ ‫البوتاسيوم‬ ‫و‬ ‫المغنيسيوم‬ ‫و‬ ‫الكالسيوم‬ ‫و‬ ‫الصوديوم‬ ‫االيونات:‬ ‫اكيز‬ ‫تر‬ ‫ة‬ ‫الهيدروكيميائية‬ ‫الصيغة‬ ‫وكذلك‬ ‫ات.‬ ‫النتر‬ ‫و‬ ‫بونات‬ ‫البيكر‬ ‫و‬ ‫نوع‬ ‫من‬ ‫كانت‬ ‫الجوفية‬ ‫االبار‬ ‫معظم‬ ‫مياه‬ ‫ان‬ (Ca-Cl) (‫و‬ SO4-Ca (‫و‬) 4 SO-Mg) (‫و‬ Cl-Na ‫الماء.‬ ‫في‬ ‫األيونات‬ ‫لهذه‬ ‫العالية‬ ‫اكيز‬ ‫التر‬ ‫بسبب‬ ‫الي‬ ‫التو‬ ‫وعلى‬) ‫غير‬ ‫المياه‬ ‫هذه‬ ‫أن‬ ‫تبين‬ ‫اقية‬ ‫العر‬ ‫اصفة‬ ‫المو‬ ‫و‬ ‫العالمية‬ ‫الصحة‬ ‫منظمة‬ ‫متطلبات‬ ‫مع‬ ‫البحث‬ ‫النتائج‬ ‫نة‬ ‫مقار‬ ‫وعند‬ ‫اني‬ ‫الحيو‬ ‫لالستهالك‬ ‫مناسبة‬ ‫انها‬ ‫اال‬ ، ‫ملوحتها‬ ‫تفاع‬ ‫الر‬ ‫ا‬ ‫نظر‬. ‫شرب‬ ‫كمياه‬ ‫البشري‬ ‫لالستهالك‬ ‫صالحة‬ ‫ألن‬ ،. et al khafaji-Al 4293 ‫ألن‬ ، ‫اإلنشائية‬ ‫اض‬ ‫لألغر‬ ‫تصلح‬ ‫أنها‬ ‫حين‬ ‫في‬ ‫مقبولة.‬ ‫حدود‬ ‫ضمن‬ ‫تقع‬ ‫الذائبة‬ ‫الصلبة‬ ‫اد‬ ‫المو‬ ‫و‬ ‫العناصر‬ ‫جميع‬ ‫اض‬ ‫لألغر‬ ‫ايضا‬ ‫صالحة‬ ‫غير‬ ‫هي‬ ‫المياه‬ ‫هذه‬ ‫أن‬ ‫وجد‬ ‫فقد‬ ‫لذلك‬ ، ‫المسموحة‬ ‫الحدود‬ ‫تتجاوز‬ ‫لم‬ ‫عناصرها‬ ‫جميع‬ ‫التي‬ ‫المحاصيل‬ ‫لري‬ ‫استخدامها‬ ‫ويمكن‬ ،.، ‫الري‬ ‫و‬ ‫الصناعية‬ ‫العالية‬ ‫الملوحة‬ ‫تتحمل‬ Introduction : Groundwater is the second main water source worldwide. The composition of groundwater is subject to the influence of many climatic factors, topography and hydrographic nature. However, the main effect on groundwater quality is through the chemical composition of the water-bearing rocks and the chemical composition of the deep water that participates in feeding the water-bearing levels located at the top and coming to it through the weak permeability separating layers [1]. Therefore, one of the most important objectives of this research is to study the hydrochemical situation prevailing in the study area, its physical and chemical properties.
... The composition of groundwater is subject to the influence of many climatic factors, topography and hydrographic nature. However, the main effect on groundwater quality is through the chemical composition of the water-bearing rocks and the chemical composition of the deep water that participates in feeding the water-bearing levels located at the top and coming to it through the weak permeability separating layers [1]. Therefore, one of the most important objectives of this research is to study the hydrochemical situation prevailing in the study area, its physical and chemical properties. ...
... The acidic function ( pH) is the negative logarithm of the concentration of the hydrogen ion, and it is considered a measure of the acidity and basicity in normal temperature and pressure [10]. The highest value pH. was in Well No. (1). This reached (8.7), and the lowest value was in Wells No. (2) (7.1). ...
Article
Full-text available
Twenty-five groundwater samples from the Al-Zubair area, southern Iraq, were analyzed for physical and chemical variables. The study showed that the groundwater is of acidic type and in it tends towards light alkalinity. Both electrical conductivity and the total dissolved solids showed increased concentrations of sodium, calcium, magnesium, potassium and sulfate, chloride, bicarbonate, and nitrate. The hydrochemical formula for most groundwater wells are (Ca-Cl), (Ca-SO4), (Mg-SO4), and (Na-Cl) type due to the high concentrations of these ions in the water., it was found that this water is not suitable for human drinking. Due to its high salinity compared to the requirements of international standard and Iraqi standard standards, while it is suitable for drinking animal's construction purposes, it has not exceeded the permissible limits. Also, it has been found that this water is not suitable for industrial and irrigation purposes, where it is possible to grow crops that tolerate high salinity ‫ل‬ ‫بيئية‬ ‫اسة‬ ‫در‬ ‫نوعية‬ ‫الزبير‬ ‫في‬ ‫المختارة‬ ‫االبار‬ ‫بعض‬ ‫في‬ ‫الجوفية‬ ‫المياه‬ ، ‫جنوب‬ ‫ي‬ ‫استعماالتها‬ ‫و‬ 2 ‫جيجان‬ ‫بتول‬ ، 1 ‫االمير‬ ‫عبد‬ ‫فاطمة‬ ، *1 ‫الخفاجي‬ ‫رعد‬ ‫اق‬ ‫العر‬ ‫بغداد،‬ ‫بغداد،‬ ‫جامعة‬ ‫الهيثم)،‬ ‫فه(ابن‬ ‫الصر‬ ‫للعلوم‬ ‫بيه‬ ‫التر‬ ‫كلية‬ ، ‫الحياة‬ ‫علوم‬ ‫قسم‬ 1 2 ، ‫الحياة‬ ‫علوم‬ ‫قسم‬ ‫ثانوية‬ ‫كلية‬ ‫بغداد،‬ ‫اق‬ ‫العر‬ ‫بغداد،‬ ‫الخالصة‬ ‫تم‬ ‫اختيار‬ 25 ‫اق‬ ‫العر‬ ‫جنوب‬ ‫بير‬ ‫الز‬ ‫منطقة‬ ‫من‬ ‫ة‬ ‫مختار‬ ‫ألبار‬ ‫الجوفية‬ ‫المياه‬ ‫من‬ ‫عينة‬ ‫المياه‬ ‫نوعية‬ ‫فة‬ ‫لمعر‬ ‫حيث‬ ‫حمضية‬ ‫اسة‬ ‫الدر‬ ‫منطقة‬ ‫في‬ ‫الجوفية‬ ‫المياه‬ ‫أن‬ ‫النتائج‬ ‫أظهرت‬ ‫الكيميائية.‬ ‫و‬ ‫يائية‬ ‫الفيز‬ ‫ات‬ ‫المتغير‬ ‫تحديد‬ ‫خالل‬ ‫بعض‬ ‫في‬ ‫الذائبة‬ ‫الصلبة‬ ‫اد‬ ‫المو‬ ‫و‬ ‫بائية‬ ‫الكهر‬ ‫التوصيلية‬ ‫من‬ ‫كال‬ ‫تركيز‬ ‫في‬ ‫يادة‬ ‫ز‬ ‫هناك‬ ‫الخفيفة.‬ ‫القلوية‬ ‫نحو‬ ‫تميل‬ ‫اس‬ ‫در‬ ‫اظهرت‬ ‫االبار.‬ ‫تلك‬ ‫مياه‬ ‫يد‬ ‫الكلور‬ ‫و‬ ‫يتات‬ ‫الكبر‬ ‫و‬ ‫البوتاسيوم‬ ‫و‬ ‫المغنيسيوم‬ ‫و‬ ‫الكالسيوم‬ ‫و‬ ‫الصوديوم‬ ‫االيونات:‬ ‫اكيز‬ ‫تر‬ ‫ة‬ ‫الهيدروكيميائية‬ ‫الصيغة‬ ‫وكذلك‬ ‫ات.‬ ‫النتر‬ ‫و‬ ‫بونات‬ ‫البيكر‬ ‫و‬ ‫نوع‬ ‫من‬ ‫كانت‬ ‫الجوفية‬ ‫االبار‬ ‫معظم‬ ‫مياه‬ ‫ان‬ (Ca-Cl) (‫و‬ SO4-Ca (‫و‬) 4 SO-Mg) (‫و‬ Cl-Na ‫الماء.‬ ‫في‬ ‫األيونات‬ ‫لهذه‬ ‫العالية‬ ‫اكيز‬ ‫التر‬ ‫بسبب‬ ‫الي‬ ‫التو‬ ‫وعلى‬) ‫غير‬ ‫المياه‬ ‫هذه‬ ‫أن‬ ‫تبين‬ ‫اقية‬ ‫العر‬ ‫اصفة‬ ‫المو‬ ‫و‬ ‫العالمية‬ ‫الصحة‬ ‫منظمة‬ ‫متطلبات‬ ‫مع‬ ‫البحث‬ ‫النتائج‬ ‫نة‬ ‫مقار‬ ‫وعند‬ ‫اني‬ ‫الحيو‬ ‫لالستهالك‬ ‫مناسبة‬ ‫انها‬ ‫اال‬ ، ‫ملوحتها‬ ‫تفاع‬ ‫الر‬ ‫ا‬ ‫نظر‬. ‫شرب‬ ‫كمياه‬ ‫البشري‬ ‫لالستهالك‬ ‫صالحة‬ ‫ألن‬ ،. et al khafaji-Al 4293 ‫ألن‬ ، ‫اإلنشائية‬ ‫اض‬ ‫لألغر‬ ‫تصلح‬ ‫أنها‬ ‫حين‬ ‫في‬ ‫مقبولة.‬ ‫حدود‬ ‫ضمن‬ ‫تقع‬ ‫الذائبة‬ ‫الصلبة‬ ‫اد‬ ‫المو‬ ‫و‬ ‫العناصر‬ ‫جميع‬ ‫اض‬ ‫لألغر‬ ‫ايضا‬ ‫صالحة‬ ‫غير‬ ‫هي‬ ‫المياه‬ ‫هذه‬ ‫أن‬ ‫وجد‬ ‫فقد‬ ‫لذلك‬ ، ‫المسموحة‬ ‫الحدود‬ ‫تتجاوز‬ ‫لم‬ ‫عناصرها‬ ‫جميع‬ ‫التي‬ ‫المحاصيل‬ ‫لري‬ ‫استخدامها‬ ‫ويمكن‬ ،.، ‫الري‬ ‫و‬ ‫الصناعية‬ ‫العالية‬ ‫الملوحة‬ ‫تتحمل‬ Introduction : Groundwater is the second main water source worldwide. The composition of groundwater is subject to the influence of many climatic factors, topography and hydrographic nature. However, the main effect on groundwater quality is through the chemical composition of the water-bearing rocks and the chemical composition of the deep water that participates in feeding the water-bearing levels located at the top and coming to it through the weak permeability separating layers [1]. Therefore, one of the most important objectives of this research is to study the hydrochemical situation prevailing in the study area, its physical and chemical properties.
... The composition of groundwater is subject to the influence of many climatic factors, topography and hydrographic nature. However, the main effect on groundwater quality is through the chemical composition of the water-bearing rocks and the chemical composition of the deep water that participates in feeding the water-bearing levels located at the top and coming to it through the weak permeability separating layers [1]. Therefore, one of the most important objectives of this research is to study the hydrochemical situation prevailing in the study area, its physical and chemical properties. ...
... The acidic function ( pH) is the negative logarithm of the concentration of the hydrogen ion, and it is considered a measure of the acidity and basicity in normal temperature and pressure [10]. The highest value pH. was in Well No. (1). This reached (8.7), and the lowest value was in Wells No. (2) (7.1). ...
Article
Twenty-five groundwater samples from the Al-Zubair area, southern Iraq, were analyzed for physical and chemical variables. The study showed that the groundwater is of acidic type and in it tends towards light alkalinity. Both electrical conductivity and the total dissolved solids showed increased concentrations of sodium, calcium, magnesium, potassium and sulfate, chloride, bicarbonate, and nitrate. The hydrochemical formula for most groundwater wells are (Ca-Cl), (Ca-SO4), (Mg-SO4), and (Na-Cl) type due to the high concentrations of these ions in the water., it was found that this water is not suitable for human drinking. Due to its high salinity compared to the requirements of international standard and Iraqi standard standards, while it is suitable for drinking animal's construction purposes, it has not exceeded the permissible limits. Also, it has been found that this water is not suitable for industrial and irrigation purposes, where it is possible to grow crops that tolerate high salinity
... Studies related to Lake Sawa have been conducted and included the chemical properties of the water and/or soil [14][15][16][17][18]. At the same time, very few studies targeted monitoring the water level changes, e.g., [4], and few morphological studies were published in the Arabic language. ...
... Remote Sens. 2022,14, 1831 ...
Article
Full-text available
Lake Sawa located in Southwest Iraq is a unique natural landscape and without visible inflow and outflow from its surrounding regions. Investigating the environmental and physical dynamics and the hydrological changes in the lake is crucial to understanding the impact of hydrological changes, as well as to inform planning and management in extreme weather events or drought conditions. Lake Sawa is a saltwater lake, covering about 4.9 square kilometers at its largest in the 1980s. In the last decade, the lake has dried out, shrinking to less than 75% of its average size. This contribution focuses on calculating the bank erosion and accretion of Lake Sawa utilizing remote sensing data captured by Landsat platforms (1985–2020). The methodology was validated using higher-resolution Sentinel imagery and field surveys. The outcomes indicated that the area of accretion is significantly higher than erosion, especially of the lake’s banks in the far north and the south, in which 1.31 km2 are lost from its surface area. Further analysis of especially agricultural areas around the lake have been performed to better understand possible reasons causing droughts. Investigations revealed that one possible reason behind droughts is related to the rapid increase in agriculture areas surrounding the lake. It has been found that the agriculture lands have expanded by 475% in 2020 compared to 2010. Linear regression analysis revealed that there is a high correlation (69%) between the expanding of agriculture lands and the drought of Lake Sawa.
... In the study area, the slope sediments that cannot be separated distinguish them from the slope sediments in the Holocene period. Likewise, the Holocene deposits are other deposits present in the study area and include depressions filling deposits and slope deposits [7]. ...
... The length of daylight hours affects the determination of the number of solar rays reaching the surface of the earth. The greater the length of time that the sun is capable of, the greater the number of rays, and vice versa [7]. The thermal characteristics of any region are the result of a set of factors, the foremost of which is the astronomical position that determines the amount of solar radiation reaching the surface of the earth, and as a result of the location of the southern desert within the western desert plateau, west of the Euphrates, that is, it is located within the arid region, which added to its characteristics to be printed with the characteristics of this dry region and that the temperatures start to rise from January to reach their highest levels in the months (June, July, August), and in the winter they fall to their lowest levels (December, January, February). ...
Article
This research examined the chemical and physical properties of the ground water in the different parts of the Samawah desert in order to assess its suitability for agricultural purposes'and whether it causes an increase in the salinization of natural pasture lands used for the purpose of agricultural production, and thus exposes them to severe desertification. Several parameters are examined for (16) wells and (3) artesian wells which are located in the different regions of Samawah desert depending on the scientfic methods of sample collection in mid-February (2019). The results showed that there are differences in the ground water aspects (chemical and physical aspects) among wells water and most of the wells water was a saline water which causes an increase in the likelihood of pasture lands being exposed to severe desertification as a result of using this water for agricultural production purposes in those lands. However, there are three wells where have a good quality of water, therefore, these three wells are suitable for agricultural uses, unlike the rest of the examined wells, where the water was not suitable for agriculture or suitable for agriculture, but taking care of the soil.
... The depth reduction has caused a decrease in the circumference of the lake from 12.3 km in 1990 to 11.4 km in 2012 (Al-Abadi 2013; Al-Mosawi et al. 2015). The water level also fluctuates during the dry and wet seasons; however, the lake does not dry up because of the equilibrium state between the groundwater discharge and evaporation (Al-Quraishi 2013; Awadh and Muslim 2014;Jamil 1977). ...
... The logfCO 2 = − 3.4 was kept fixed, and to simulate evaporation, H 2 O was progressively removed by solution to obtain a final chloride concentration similar to the lake (~ 10 g/l). According to the mineralogical investigation of the lake sediments and surrounding barrier (Al-Quraishi 2013; Awadh 2016; Awadh and Muslim 2014;Naqash et al. 1977), gypsum is the main mineral produced during evaporation, whereas calcite is a minor phase. Despite the dolomite and magnesite oversaturation, their precipitation was suppressed during the modeling. ...
Article
Full-text available
The examination of past and new chemical–isotopic data (2H/1H–18O/16O, 11B/10B and 87Sr/86Sr ratios) shows the meteoric origin of the Sawa Lake (Muthanna Governorate, Iraq) and its connection with the local aquifers, which feed the lake via the groundwater emerging from its floor through fault systems. The chemical and isotopic evaporation models are traced by geochemical computer codes by using a different composition of some potential inflows to the lake (e.g., the Euphrates River and Dammam aquifer). The main product of the chemical evaporation models is gypsum, as confirmed by the mineralogical examination of the sediment and the surrounding outcrops. A strong 18O–2H enrichment is a consequence of the evaporation effect in arid regions; δ18O–Cl models and δ11B = + 23.4‰ exclude the contribution of any seawater-derived fluids. This latter value along with 87Sr/86Sr = 0.707989 suggests a mixed origin from the Eocene–Miocene aquifers. The isotope and chemical evaporation paths from the meteorically recharged sources match the lake composition. However, compositional switches from NaCl toward MgCl2 occurred in the last decade and are related to post-drought periods, showing that the interaction of the recharging waters with the local soils (Na–Mg exchange and/or the leaching of the top layer salts) have a role in the chemical composition. This demonstrates that the lake is significantly influenced by climatic variations
... Accordingly, set of springs emerged to the surface. The AJFZ is a fault basin provides many oil seepages to the surface [1], [2] and [3]. The location of theses seepages is clearly tectonically controlled [4]. ...
... Hydrogeochemical studies throughout the AJFZ demonstrated that the spring water is a marine origin composed from mixture of oil field and meteoric waters [1], [2] and [3]. Alkans, polycyclic alphatics and polycyclic aromatic hydrocarbons can be used for describing the characterization of oil source [5]. ...
Article
Oil seep samples along Abu-Jir Fault Zone were studied to determine their chemical characterization and origin. They are dominated by the normal alkanes, more complex mixture of branched and cyclic hydrocarbons. Organofacies coupled with the stable carbon isotopes have been integrated to infer the oil seep origin. Oil seeps contain H2S gas, which derives as a catabolic by product of sulfate-reducing bacteria from gypsum of the Fatha Formation during the early diagenetic under anoxic conditions which is demonstrated by values of C29/H that are greater than 1. The oil seeps are characterized by δ13C values vary from -29.0 to -27.96‰ and from -28.34 to -27.88‰ in the saturated and aromatic compounds, respectively; consequently, they have low values of the canonical variable ranged from -3.47 to -0.17 reflecting a marine non-waxy oil generated from planktonic kerogen of type-II that has been partially mixed with the terrestrial origin. The values of the tricyclic terpanes (C22/C21 and C31R/H) that are higher than 0.5 and 0.25 respectively support the marine source rocks. The Triassic age was suggested for the oil age in the dependence of the occurrence of the aromatic dinosteranes which marked dinoflagellates were participated in the oil derivation.
... Accordingly, set of springs emerged to the surface. The AJFZ is a fault basin provides many oil seepages to the surface [1], [2] and [3]. The location of theses seepages is clearly tectonically controlled [4]. ...
... Hydrogeochemical studies throughout the AJFZ demonstrated that the spring water is a marine origin composed from mixture of oil field and meteoric waters [1], [2] and [3]. Alkans, polycyclic alphatics and polycyclic aromatic hydrocarbons can be used for describing the characterization of oil source [5]. ...
Article
Oil seep samples along Abu-Jir Fault Zone were studied to determine their chemical characterization and origin. They are dominated by the normal alkanes, more complex mixture of branched and cyclic hydrocarbons. Organofacies coupled with the stable carbon isotopes have been integrated to infer the oil seep origin. Oil seeps contain H 2 S gas, which derives as a catabolic by product of sulfate-reducing bacteria from gypsum of the Fatha Formation during the early diagenetic under anoxic conditions which is demonstrated by values of C29/H that are greater than 1. The oil seeps are characterized by δ 13 C values vary from-29.0 to-27.96‰ and from-28.34 to-27.88‰ in the saturated and aromatic compounds, respectively; consequently, they have low values of the canonical variable ranged from-3.47 to-0.17 reflecting a marine non-waxy oil generated from planktonic kerogen of type-II that has been partially mixed with the terrestrial origin. The values of the tricyclic terpanes (C22/C21 and C31R/H) that are higher than 0.5 and 0.25 respectively support the marine source rocks. The Triassic age was suggested for the oil age in the dependence of the occurrence of the aromatic dinosteranes which marked dinoflagellates were participated in the oil derivation.
... Accordingly, set of springs emerged to the surface. The AJFZ is a fault basin provides many oil seepages to the surface [1], [2] and [3]. The location of theses seepages is clearly tectonically controlled [4]. ...
... Hydrogeochemical studies throughout the AJFZ demonstrated that the spring water is a marine origin composed from mixture of oil field and meteoric waters [1], [2] and [3]. Alkans, polycyclic alphatics and polycyclic aromatic hydrocarbons can be used for describing the characterization of oil source [5]. ...
Article
Oil seep samples along Abu-Jir Fault Zone were studied to determine their chemical characterization and origin. They are dominated by the normal alkanes, more complex mixture of branched and cyclic hydrocarbons. Organofacies coupled with the stable carbon isotopes have been integrated to infer the oil seep origin. Oil seeps contain H 2 S gas, which derives as a catabolic by product of sulfate-reducing bacteria from gypsum of the Fatha Formation during the early diagenetic under anoxic conditions which is demonstrated by values of C29/H that are greater than 1. The oil seeps are characterized by δ 13 C values vary from-29.0 to-27.96‰ and from-28.34 to-27.88‰ in the saturated and aromatic compounds, respectively; consequently, they have low values of the canonical variable ranged from-3.47 to-0.17 reflecting a marine non-waxy oil generated from planktonic kerogen of type-II that has been partially mixed with the terrestrial origin. The values of the tricyclic terpanes (C22/C21 and C31R/H) that are higher than 0.5 and 0.25 respectively support the marine source rocks. The Triassic age was suggested for the oil age in the dependence of the occurrence of the aromatic dinosteranes which marked dinoflagellates were participated in the oil derivation.
... Alternatively, it is possible that P. abu might have reached Sawa Lake prior to their deliberate introduction in 2008 from the nearby lakes, such as Al-Tharthar Dam Lake and Razzazh Lake (Epler et al., 2001), via waters of the Euphrates River running through aquifers within the Euphrates Formation. Either way, it now seems that P. abu has become established in the Sawa Lake (Ahmed et al., 2008; Awadh & Muslim, 2014). The latter scenario may also explain the presence of Aphanius dispar within Sawa Lake (Ahmed et al., 2008). ...
... Although Acentrogobius dayi has not previously been recorded from Sawa Lake, this may simply be due to the lack of appropriate ichthyological investigation methodologies . Previous investigations were mainly concerned with the lake's geology (Jamil, 1977; Naqash et al., 1977; Awadh & Muslim, 2014). The current ichthyological investigation was the first time that scuba diving and specimen collection was included. ...
Article
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Three adult specimens of the fish species Acentrogobius dayi were collected from Sawa Lake, south-west of Baghdad, Iraq. The current report represents the first record of A. dayi from Sawa Lake and from other inland water bodies of Iraq.
... In Malaysia, water quality is determined based on National Water Quality Standards for Malaysia (NWQS). Natural water pollution is identified from single sources such as drainage, water discharge, and roads or non-point sources such as rainwater and runoff into nearby lakes or rivers (Viman et al., 2010;Awadh and Muslim, 2014). The problems associated with lakes include algae bloom, foul smells, aquatic plants, and turbidity due to the destruction of the ecosystem in the lake's surrounding area (Skotte and Skoglund, 2022). ...
Article
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In recent years, Universiti Tun Hussein Onn Malaysia has experienced several developments in buildings and road construction. A stormwater retention pond was built as a part of the construction plan to prevent the occurrence of floods downstream of the development sites. However, poor monitoring and maintenance of the pond caused water contamination, which had bad effects on the nearby environment and lake ecosystem. Therefore, this study was conducted to assess the current water quality in the pond by using a combination between Multispectral Unmanned Aerial Vehicle images and in-situ sampling. Four water quality parameters were investigated, namely turbidity, dissolved oxygen, temperature, and pH. Aerial images were taken using a multispectral aerial mapping camera attached to UAV. The in-situ testing was performed on the same day of image capturing at 5 different locations. According to the results, it was found that the pH and water temperature were within the normal levels with maximum and minimum values of 7.34 and 6.94 for pH and 28.39oC and 28.04oC for temperature, respectively. Turbidity readings appaired with a significant variation with a maximum value of 30.9 NTU at the lake outlet and a minimum value of 18.8 NTU at the middle of the lake. Dissolved oxygen concentration was noticed to be low, with an average value of 4.3 mg/l. Water quality mapping showed the concentration distribution of each water quality parameter along the lake surface. In each map, the differences in terms of colours were found to be not significant because of the size of the lake, which is relatively small, as well as because of the small differences in terms of water quality ridings at each sampling point.
... This phenomenon is attributed to the proximity of groundwater to the surface (Friedman, 1978;Hsü, 2013;). Sabkha means salinization of the soil, which in itself is a phenomenon that arises due to the high level of shallow groundwater (Quraishi et al. 2013; Awadh and Muslim, 2014;Awadh et al., 2016), and the poorly permeable soil prevents water from leaching during conventional irrigation, so it is not rinsed (Awadh and Al-Hamdani, 2019). Compared to regular seawater, the salt concentration in the Sabkha and water is typically several times higher. ...
Article
The study aims to detail the chemistry of Sabkha located in Abu-Graib, western Baghdad to know the content of the rare elements distributed. Sabkhas are found in dry areas with significant evaporation rates. The quantity of dissolved salts rises as water evaporates from the shallow basins, eventually causing salt to crystallize. The creation of the distinctive salt pans and crusts on the top is greatly influenced by this process. The trace elements (Ti, V, Cr, Mn, Ni, Cu, Zn, Ga, As, Se, Rb, Sr, Y, Zr, Nb, Mo, Sn, Ba, Ta, Tl, Pb, Th, U, I, and Br) beside the major oxides were analyzed using XRF technique. There are no clear significant differences in the distribution of the elements between the two Sabkhas in the village of Kadim Alaa’ab and the village of Haj Shiaa. Sabkhas are characterized by limited oxygen supplies in the brine, high temperatures, and precipitation of evaporite minerals including chlorides, sulfates, and sulfides. Halite predominates in the Sabkha sediments due to the association of chloride with Na2O. The CaO is distributed forming calcite, dolomite and gypsum as well as a small amount of clay minerals. The association of trace elements, especially Ni, Rb, Ta, Tl and Br, is mainly concentrated with clay minerals, followed by their concentration in silica, especially Y, Zr and Th. As for halite, it is not associated with trace elements.
... The oxygen content of natural water is an important factor in the distribution and growth of parasites, as the dissolved oxygen values are affected by several factors, including temperature, abundance of aquatic plants, wind speed, and the amount of organic matter, Also results of this current study shown an increase in values of the dissolved oxygen during the spring, and this is due to the lower temperatures that are backward proportional to the dissolution of gases in the water, as well as the lack of decomposition of organic matter [34]. As for the decrease in dissolved oxygen values during the summer, it may be due to the increase in temperature, which increases the level of decomposition of organic matter due to the increase in parasite activity and thus the consumption of dissolved oxygen [35]. Salinity is one of the important environmental factors that determine the presence and distribution of parasites, and that the increase and decrease in salinity affects physiological actions, regardless of the extent of their pollutant effect [36]. ...
Article
Full-text available
In order to know the efficiency of sterilization in eliminating parasites and its suitability for environment measurements, samples of the water and sediments was taken from six stations the Euphrates River. The samples were transported in clean and sterile bottles to the laboratory. A sedimentation method was used for parasites. Ten species of parasites isolated from water of the six stations while isolated seven were exists in the sediments of these stations. The water and sediments of the station first were contaminate with parasites rate 25.8% and 13.7%, the water and sediments of the second station are contaminated with parasites rate 12.8% and 20.2%, the water and sediments of the third station are contaminated with parasites rate 4.2% and 18.2%, the water and sediments of the fourth station are contaminated with parasites rate 22.8% and 18%, the water and sediments of the fifth station are contaminated with parasites rate 12.0% and 5.4% and the water and sediments of the sixth station are contaminated with parasites rate 12.9% and 1.7%. Giardia lamblia rate 25.4% it is most found in water while Trichomonas hominis rate 18.4% It is most found in sediments. A result of the study shows significant difference between of the temperature of air and water in all study stations, the air temperature ranged (40.10-15.2°C) and the water temperature between (26.3-9.4°C) while PH was (9.89-7.5), recorded electrical conductivity (5745-2515 ls/cm) and salinity was (4.80-1.56 g/cm) the river's water was of low salinity also dissolved oxygen was (12.9-6.2 mg/L). Date seed used as granular by activated carbon used for purification and remove parasite from water filter and waste water treatment.
... al and stable isotopic properties of groundwater and its relationship to the surface water of Muthanna Governorate in southern Iraq (Al-Naseri and Abdul-Razzaq, 2015). Their conclusion revealed that there were no groundwater effects on the quality of the surface water in Al-Atshan River. Fig. 2. Geological map of the study area and its surrounding (Awadh, et. al, 2014) ...
Article
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This study aims to use the environmental isotopes technique to evaluate the interaction between groundwater and surface water at a location between two cities in the southwest of Iraq; namely Al-Kifl and Al-Samawa. The salinity of the Euphrates River water increases sharply as it passes in this area, to a level that affects its usage for municipal purposes. A total of 111 samples were collected from the rivers, drainages, springs, shallow and deep wells, and from Sawa Lake, and all the samples were subjected to chemical (TDS, SO4, Cl, and B) and isotopic (deuterium and oxygen-18) analyses. The chemical and isotopic results showed no interference between the quality of the groundwater (from wells and springs) and Sawa Lake water with the Euphrates River water, in the study area, and hence, neither the groundwater nor Sawa Lake affects the river water quality. Statistically, the t-test analysis showed significant differences among those water samples (p-values less than 0.05 for almost all the chemical and isotopic parameters). On the other hand, drainage water showed a strong relationship to the river water, which indicates a high and strong influence of the drainage water on the river water quality when it mixes with the Euphrates River water.
... Cadmium enters natural systems through wastewater and may be sourced from some industries such as paints, battery production, dyes, etc (Awadh and Yousif, 2015;Awadh and Al-Jubury, 2015). Cadmium was found in high concentration in different water types (Awadh and Muslim, 2014;Awadh and Yousif, 2015). Cadmium and some heavy metals were tested to be removed from the aqueous solutions by many researchers for instance, Awadh and Abdulla (2017) studied the purification of aqueous solutions from Pb (II) by natural bentonite. ...
Article
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This research aims to test the ability of glass waste powder to adsorb cadmium from aqueous solutions. The glass wastes were collected from the Glass Manufacturing Factory in Ramadi. The effect of concentration and reaction time on sorption was tested through a series of laboratory experiments. Four Cd concentrations (20, 40, 60, and 80) as each concentration was tested ten times for 5, 10, 15, 20, 25, 30, 35, 40, 45, and 50 min. Solid (glass wastes) to liquid was 2g to 30ml was fixed in each experiment where the total volume of the solution was 30ml. The pH, total dissolved salts and electrical conductivity were measured at 30ºC. The equilibrium concentration was determined at 25 minutes, thereafter it was noted that the sorption (%) decreased whenever increasing Cd concentration. Langmuir and Freundlich's equations showed that the sorption intensity is 2.402 and the adsorption capacity is 3.126, and the sorption of Cd fits with the Freundlich equation. Consequently, it was clarified how glass waste material can be utilized for reducing the high levels of Cd concentrations from aqueous solutions as a step to combat environmental pollution.
... The sources of salts and their mineral components in Iraq were determined with an estimate of the salt reserves (Jassim and Al-Badri, 2019). Many lakes formed due to structural depression defined as a sag pond (Awadh and Muslim, 2014;Awadh. 2016;Boschetti et al., 2020). ...
Article
The research aims to study Sabkha mineralogy to determine the mineral types, the nature of the precipitation, and the patterns of salt crystallization. Two Sabkhas in Abu Ghraib, west of Baghdad, were studied. It was found that the Sabkhas were formed in flat ponds from saturated solutions in a semi-arid to arid climate. Halite predominates, followed by anhydrite and gypsum as evaporite minerals. As for the minerals of the Sabkha soil, it consisted of feldspar, calcite, quartz, and dolomite, in addition to the clay minerals represented by kaolinite, illite, and chlorite. Needle forms, hopper shapes, dendritic crystals, and polygon shapes are the main crystallization patterns dominantly found in the Sabkhas. All these types of crystallization occurre under normal temperatures.
... The oxygen content of natural water is an important factor in the distribution and growth of parasites, as the dissolved oxygen values are affected by several factors, including temperature, abundance of aquatic plants, wind speed, and the amount of organic matter, Also results of this current study shown an increase in values of the dissolved oxygen during the spring, and this is due to the lower temperatures that are backward proportional to the dissolution of gases in the water, as well as the lack of decomposition of organic matter [34]. As for the decrease in dissolved oxygen values during the summer, it may be due to the increase in temperature, which increases the level of decomposition of organic matter due to the increase in parasite activity and thus the consumption of dissolved oxygen [35]. Salinity is one of the important environmental factors that determine the presence and distribution of parasites, and that the increase and decrease in salinity affects physiological actions, regardless of the extent of their pollutant effect [36]. ...
Article
Full-text available
In order to know the efficiency of sterilization in eliminating parasites and its suitability for environment measurements, samples of the water and sediments was taken from six stations the Euphrates River. The samples were transported in clean and sterile bottles to the laboratory. A sedimentation method was used for parasites. Ten species of parasites isolated from water of the six stations while isolated seven were exists in the sediments of these stations. The water and sediments of the station first were contaminate with parasites rate 25.8% and 13.7%, the water and sediments of the second station are contaminated with parasites rate 12.8% and 20.2%, the water and sediments of the third station are contaminated with parasites rate 4.2% and 18.2%, the water and sediments of the fourth station are contaminated with parasites rate 22.8% and 18%, the water and sediments of the fifth station are contaminated with parasites rate 12.0% and 5.4% and the water and sediments of the sixth station are contaminated with parasites rate 12.9% and 1.7%. Giardia lamblia rate 25.4% it is most found in water while Trichomonas hominis rate 18.4% It is most found in sediments. A result of the study shows significant difference between of the temperature of air and water in all study stations, the air temperature ranged (40.10-15.2°C) and the water temperature between (26.3-9.4°C) while PH was (9.89-7.5), recorded electrical conductivity (5745-2515 ls/cm) and salinity was (4.80-1.56 g/cm) the river's water was of low salinity also dissolved oxygen was (12.9-6.2 mg/L). Date seed used as granular by activated carbon used for purification and remove parasite from water filter and waste water treatment.
... Moreover, it has an additional value due to its distinctive nature. The water of Sawa Lake is originated from a set of springs located at the bottom of the lake in balance with the evaporation, which prevents its overflow (Awadh and Muslim 2014;Al-Mosawi et al. 2015;Khayyun and Minaty 2018). ...
Article
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Sawa Lake is a historical, cultural, and environmental landmark of great importance in education and tourism. Its unique advantages make it a potential global natural heritage and geopark in 2021. The current research is devoted to investigate and assess the actual reasons behind the rapid decline of the water level of Sawa Lake, which has begun to drop dramatically in an unprecedented situation. Landsat data are employed for interpreting the temporal and spatial changes of both water and vegetation covers. Shuttle Radar Topography Mission data are used for water volume estimation. Standardized Precipitation Evapotranspiration Index was used in comparing the rainfall rate to the changing of land use-land cover. Additionally, the Modified Normalized Difference Water Index and Normalized Difference Vegetation Index are established on the Landsat OLI imageries using ENVI 5.3 software. The data analysis showed that one of the most important reasons for the Sawa Lake water level drop is the massive pumping of the groundwater from a site located to the south of the lake to feed the Mamlahat Al-Samawa from which NaCl is extracted.
... The exposed formations in the study area are Ghar and Nfayil formations (Early Miocene to Middle Miocene respectively) which are composed of sedimentary rocks (Fig. 2). The Euphrates, Nfayil, Injana and Dibdibba formations cropping out in the zone of Abu jir fault, is good evidence for interpreting the fault activity (Al-Dabbas et al., 2013;Awadh, 2014;Awadh and Muslim, 2014;Awadh el.al. Awadh, 2018;Al-Dabbas et al., 2019;Awadh and Al-Owaidi, 2020). ...
Article
The research aims to assess the claystone exposed in the Nfayil Formation (Middle Miocene) for Portland cement (P.C.) manufacturing based on mineralogy and geochemistry. The importance of the study is to avoid the miming of the agricultural soils that are mining now for the cement industry. Claystones of Nfayil Formation and the limestone of the Euphrates Formation were used to design the raw mixture as clay to limestone (1:3). The chemical composition (%) of the designed mixture was calculated using the Alligation Alternative Method (A.A.M.) as CaO (65.52), MgO (1.05), SiO2 (21.65), Al2O3 (7.43), Fe2O3 (2.62), Na2O3+K2O (1.52) and SO3 (0.26), which are suitable for P.C. The lime saturation factor (LSF = 92.8), silica saturation factor (SSF = 0.87), alumina ratio (AR = 2.8), silica ratio (SR = 2.16), and calcium to silica (CS = 3.04) of the planned mixture are all within the permissible range. A clinker was successfully manufactured as composed mainly of belite, alite, aluminate, and ferrite.
... The only ways to gain or lose water are by rainfall, evaporation, or groundwater. Some algae species, phytoplankton, and a few kinds of fish exist (Awadh & Muslim, 2014;Hassan et al., 2006). Hence, fish species need to be preserved in the lake to meet the human essentials (Cordier et al., 2020;Moayedi et al., 2019). ...
Article
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An integrated linear regression technique was developed and validated to model dissolved oxygen in salt lakes by using R software and based on data from Sawa Lake, Iraq. The technique helps understand and evaluate salty aquatic ecosystems in the presence of water quality data gaps. The technique involved selecting the important water quality parameters that have significant statistical relationship with dissolved oxygen. In order to make the regression development simpler, the validation approach was incorporated with the model. Linearity, homogeneity, normality, outliers, and influential data points were verified. The simulation approach was also capable of displaying the interaction between the selected water quality parameters and the other insignificant parameters. The statistical analysis results indicated that dissolved oxygen in salt lakes is a function of total dissolved solids. The developed model represented dissolved oxygen with R-squared of 90.73% and p-value of 1.08E-06. Furthermore, the model results showed that the influence of salty ions on dissolved oxygen/total dissolved solids model is the same. It was found that temperature has a significant impact on the developed dissolved oxygen model. In addition, the model simulation revealed that salt melting surrounding the lake due to temperature variation during the year cycle increased total dissolved solids in the lake water. Consequently, the lake dissolved oxygen levels were impacted.
... The oxygen content of natural water is an important factor in the distribution and growth of parasites, as the dissolved oxygen values are affected by several factors, including temperature, abundance of aquatic plants, wind speed, and the amount of organic matter, Also results of this current study shown an increase in values of the dissolved oxygen during the spring, and this is due to the lower temperatures that are backward proportional to the dissolution of gases in the water, as well as the lack of decomposition of organic matter [34]. As for the decrease in dissolved oxygen values during the summer, it may be due to the increase in temperature, which increases the level of decomposition of organic matter due to the increase in parasite activity and thus the consumption of dissolved oxygen [35]. Salinity is one of the important environmental factors that determine the presence and distribution of parasites, and that the increase and decrease in salinity affects physiological actions, regardless of the extent of their pollutant effect [36]. ...
Article
Full-text available
أجريت هذه الدراسة في البيت الحيواني لقسم علوم الحياة/ كلية التربية للبنات / جامعة الكوفة للمدة من شهر تشرين الاول 2016 لغاية شهر ايار 2017 تضمنت الدراسة استعمال 72 من الارانب البيض المختبرية نوع Oryetolagus cuniculus.L. وقد قسمت إلى ( 4) مجاميع لكل مجموعة ( 18 ) ارنب حيث حقنت بمضاد ( السيبروفلوكساسين Ciprofloxacin ) بتركيز مقداره (1 ملغم/كغم) من وزن الجسم أما البكتريا فكانت الجرعة ( 1ملغم /كغم) من وزن الجسم ولمدة أسبوع ، أسبوعين ، واربعة اسابيع على التوالي , بعد انتهاء فترة التجريع والحقن لكافة حيوانات التجربة تم قتلها وتشريحها لغرض الدراسة النسيجية التي تضمنت دراسة الجهاز التناسلي الانثوي وكذلك تم اخذ عينات من الدم لغرض حساب بعض المعايير الدموية والكيموحيوية. أظهرت نتائج التحليل الاحصائي عند مستوى احتمالية (P<0.05) أن المضاد الحيوي (السيبروفلوكساسين) احدث تغيرات وزنية المتمثلة بحصول انخفاض معنوي (P<0.05) في معدل الوزن الكلي في الجسم ومعدل وزن المبيض في الاناث .بينت نتائج التحليل الاحصائي لدراسة ان الحقن العلاجية المفردة لعقار (السيبروفلوكساسين) وتجريع البكتريا متباينة في تأثيرها على بعض المعايير الدموية حيث لم تظهر المجاميع المعاملة بالعقار والبكتريا تغيرات في الاسبوع الاول والثاني بينما كان هناك انخفاضا معنويا وتحت مستوى احتمالية (P<0.05) في الأسبوع الرابع متمثل بانخفاض معنوي (P<0.05) في عدد كريات الدم البيض WBC و الحمر(RBCs) ومستوى خضاب الدم (Hb) مقارنة بمجموعة السيطرة. بينت الدراسة النسيجية للمقاطع النسيجية باستخدام المجهر الضوئي حصول تغيرات نسيجية مرضية في المبيض في الاناث مختلفة الشدة والظهور بين العقار والبكتريا مقارنة بمجموعة السيطرة حيث أظهرت نتائج الفحص المجهري التأثيرات الواضحة على التركيب النسجي للمبيض في الاناث مقارنة مع مجموعة السيطرة .
... There were some variations among the different localities in the values which may be due to the different input of the agricultural and discharge along the Bahr Al-Najaf as well as the different population densities. The recorded results are lower than Awad's (2014) who registered Mn value ranging between 0.04 to 0.87 ppm in Sawa Lake. ...
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The present study was conducted to evaluate some physical and chemical parameters such as (water temperature, pH, turbidity, total dissolved solids, electrical conductivity, salinity, dissolved oxygen, biological oxygen demand, total hardness, calcium and magnesium hardness, and sulfate ions) and the concentrations of some heavy metals such as (Zinc, Lead, Cadmium, Manganese and Iron) in water of Bahr Al-Najaf. Five sites were chosen in Bahr Al-Najaf; the samples were monthly collected from April 2017 to March 2018. The results showed that water temperature ranged between (12.3-37.8) C 0 , pH values (7.16-8.88), electrical conductivity (EC)(3.8-77.8) ms/cm, salinity (2.43-49.79) ppt turbidity (Tur) (7.16-45.5) NTU, total dissolved solids(TDS)(2476-32366) mg/l, total hardness (TH) (553.18-2073)mg/l, calcium(Ca +2) and magnesium (Mg +2)ions (122.91-689.37) and (80.29-609.21) mg/L respectively, sulfate ions (SO 4)-2 (360.9-1263.1)mg/l, dissolved oxygen (DO) (6.6-17.8) mg/l, biochemical oxygen demand (BOD 5) (0.73-12.77) mg/l. The study results of heavy metals concentrations in water showed that Zinc (Zn) ranged between (0.001-13.86) ppm, lead (Pb) (0.02-1.87) ppm, cadmium (Cd) (0.001-3.33) ppm, manganese (Mn) (0.006-0.23) ppm, iron (Fe) (0.03-0.91) ppm. The water quality of Bahr Al-Najaf depression under this study was considered of salinity, slightly alkaline, very hard and concentrations of BOD 5 were recorded in some months exceeding the permissible limit. It seems clearly that Bahr Al-Najaf depression was contaminated by domestic sewage. Increasing levels of heavy metals in Bahr Al-Najaf depression exceeded the permissible limit, giving a hint of water pollution by heavy metals.
... There were some variations among the different localities in the values which may be due to the different input of the agricultural and discharge along the Bahr Al-Najaf as well as the different population densities. The recorded results are lower than Awad's (2014) who registered Mn value ranging between 0.04 to 0.87 ppm in Sawa Lake. ...
Article
Full-text available
The present study was conducted to evaluate some physical and chemical parameters such as (water temperature, pH, turbidity, total dissolved solids, electrical conductivity, salinity, dissolved oxygen, biological oxygen demand, total hardness, calcium and magnesium hardness, and sulfate ions) and the concentrations of some heavy metals such as (Zinc, Lead, Cadmium, Manganese and Iron) in water of Bahr Al-Najaf. Five sites were chosen in Bahr Al-Najaf; the samples were monthly collected from April 2017 to March 2018. The results showed that water temperature ranged between (12.3-37.8) C 0 , pH values (7.16-8.88), electrical conductivity (EC)(3.8-77.8) ms/cm, salinity (2.43-49.79) ppt turbidity (Tur) (7.16-45.5) NTU, total dissolved solids(TDS)(2476-32366) mg/l, total hardness (TH) (553.18-2073)mg/l, calcium(Ca +2) and magnesium (Mg +2)ions (122.91-689.37) and (80.29-609.21) mg/L respectively, sulfate ions (SO 4)-2 (360.9-1263.1)mg/l, dissolved oxygen (DO) (6.6-17.8) mg/l, biochemical oxygen demand (BOD 5) (0.73-12.77) mg/l. The study results of heavy metals concentrations in water showed that Zinc (Zn) ranged between (0.001-13.86) ppm, lead (Pb) (0.02-1.87) ppm, cadmium (Cd) (0.001-3.33) ppm, manganese (Mn) (0.006-0.23) ppm, iron (Fe) (0.03-0.91) ppm. The water quality of Bahr Al-Najaf depression under this study was considered of salinity, slightly alkaline, very hard and concentrations of BOD 5 were recorded in some months exceeding the permissible limit. It seems clearly that Bahr Al-Najaf depression was contaminated by domestic sewage. Increasing levels of heavy metals in Bahr Al-Najaf depression exceeded the permissible limit, giving a hint of water pollution by heavy metals.
... High salinity water is dominated the lake and the equilibrium between evaporation and the pressure gradients in the source aquifers led to the stability of water level [14]. The lake sediments are mainly consisting of gypsum (87%), clay minerals (5.5%), quartz (4.5%) and halite (3%) [15]. The vicinity of the lake is covered by recent alluvial sediments that vary in thickness between 1 to 10 m. ...
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Heavy metal contamination comprises a great concern in environment. A magnetic study combined with heavy metal analyses was performed in the Sawa Lake in Al-Muthanna governorate (southern Iraq). Concentrations of selected heavy metals (Cr, Fe, Ni, As and Pb) has been measured and magnetic susceptibility (χ) of sediment samples collected from the lake bottom was calculated. The results confirmed that a cement plant, which is located less than two kilometres away from the lake has no contamination levels on the lake’s sediments. No enhancement in the magnetic susceptibility was observed. X-ray florescence (XRF) was performed for heavy metal analyses. Spatial variations of χ with mean value of 4.58 x 10−8 m3kg−1 and results of other magnetic parameters suggest the magnetic carriers are predominantly hard magnetic phase like hematite and existence of small super-paramagnetic proportions. XRF analyses show average concentrations of (Cr, Fe, Ni) and very low for (As, Pb) which is typical for relatively clean areas. Magnetic susceptibility was insignificant correlated with heavy metals due to low concentrations of both magnetic signals and heavy metal contents. This study has shed some light on the importance of applying the χ measurements techniques to monitor and assess lakes sediment pollution.
Chapter
Mesopotamia, a Greek term for the region between the Euphrates and Tigris rivers, is the name given to Iraq. These rivers originate in the northern Anatolian highlands, join, and flow into the Arabian Gulf. The earliest civilizations were in Iraq. Its territory is densely packed with numerous, diverse archaeological sites. The civilizations of Ur, Akkadian, Sumerian, Babylonian, Assyrian, Aramaic, Islamic, the Ziggurat, the city of Hatra, the Iwan of Khosrow, the Malawiyya, the Mustansiriya School, the Tower of Babel, and the Ishtar Gate are a few examples of prehistoric and posthistoric civilizations that existed in Iraq. Each of these civilizations left its distinct imprint. Ancient Mesopotamian civilizations like the Sumerian, Akkadian, Assyrian, Babylonian, and Chaldean (Neo-Babylonian) built magnificent cities, put in place governmental frameworks, and created techniques for agriculture, writing, mathematics, and astronomy. From here, it is obvious that Iraq is home to ancient civilizations’ archaeological sites, which have left behind a rich legacy that has attracted tourists’ attention. Action must be taken to promote tourism to these sites that are compatible with the environment and geodiversity. This chapter’s attempt to cover the most significant geotourism destinations focuses on the exceptional Kurdistan region in northern Iraq. Because of its scarcity or absence, readers in the Middle East or Arab readers in particular may have difficulty finding studies, research, and references that are explicitly focused on geotourism. A beginner may struggle to understand the practical side of geotourism due to his lack of familiarity with the objectives and benefits of the specialization. These and other factors inspired the author to write this chapter as a must-have reference and how-to guide for both novice and experienced researchers. With this project, we hope to raise awareness of geotourism in the country, which is well-known around the world but underappreciated locally. The development of geotourism thinking will aid in the long-term development of geological sites. This chapter looks at potential geoparks, geotourism development strategies, and the links between geoparks and natural heritage. Through its aesthetic, social, economic, scientific, and security features, it emphasizes the critical elements of this specific tourism pattern. These goals included educating visitors about the geological features around them, encouraging them to travel in a way that preserves the site’s geographic character, and improving the site’s tourist, scientific, cultural, and economic value to promote sustainable development for the local population. This chapter draws upon the previous publication, “Geotourism in The Middle East,” which in turn is based on the author’s earlier works.
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Accurate determination of reaeration coefficient in lakes is a key factor for accurate modeling of dissolved oxygen. This study developed a new numerical model to determine the lake reaeration coefficient of Sawa lake, Iraq based on solving the transform mechanisms of dissolved oxygen without the using the empirical and laboratory methods. The model solved the gas transport at the water-air surface numerically to predict the dissolved oxygen and the reaeration coefficient simultaneously. Results showed that the lake reaeration coefficient was 0.001 day-1 at 20 °C with low root mean squared errors (0.138, 0.137, and 0.168 mg/L for the three years of simulation 2007, 2012, and 2017, respectively) and absolute mean errors (0.121, 0.114, and 0.145 mg/L in 2007, 2012, and 2017, respectively). It was noticed that the lake habitat was impacted causing unhealthy conditions (low reaeration rate), and there was upward dissolved oxygen movement due to the presence of positive trend in the yearly cycle of temperature. In addition, including this numerical approach along with other water quality models can improve the predictions of other water quality parameters.
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Sawa Lake is one of the most important tourist lakes in Iraq. It is a closed lake located in the southern plateau of Iraq in the arid region. Most of its feeding is groundwater, and there is no clear surface water source feeding it. A topographic survey was conducted for the first time for the rocky cliff, bottom and coasts of lake, Three water springs feeding it were discovered which have distinctive geomorphic characteristics located in the middle of the lake stems from distant depths. High-resolution topographic equipment (2 mm) were used in topographic lift operations. These data have been collected, processed and integrated by using ARC GIs10.2.1. First-time topographic maps of the Lake Bottom, Coast, Rocky Cliff and surrounding areas have been produced based on sea level rise, as well as follow-up of their levels depending on benchmark point. Results of the survey showed topographic differences between the earth's surface, which ranged between 18.6 - 9m, and the serious decline of water levels were also identified. In this study, which lasted for six years (2012-2017), it was proven that the lake's level declined from 15.77 m on 17 / 11/2012 to retreat to (13.80 m) on 17/11/2017.
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Experiments indicate that gypsum can be precipitated by the mixing of seawater brines of different stages of evaporation, in addition to the previously recognized mechanisms of direct evaporative crystallization and crystallization due to temperature changes. A proposed geologic model shows how gypsum precipitation by brine mixing might occur in an evaporative basin. Among conclusions drawn based on the experiments and their relations to he geologic model are precipitation occurs without further water loss by evaporation; precipitation can occur from a brine that was undersaturated before mixing; the only form of calcium sulfate to precipitate in these experiments was gypsum; and brine mixing could cause different salts to be deposited simultaneously in different parts of a basin. Refs.
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The chemical composition of natural water is derived from many different sources of solutes, including gases and aerosols from the atmosphere, weathering and erosion of rocks and soil, solution or precipitation reactions occurring below the land surface, and cultural effects resulting from human activities. Broad interrelationships among these processes and their effects can be discerned by application of principles of chemical thermodynamics. Some of the processes of solution or precipitation of minerals can be closely evaluated by means of principles of chemical equilibirum, including the law of mass action and the Nernst equation. Other processes are irreversible and require consideration of reaction mechanisms and rates. The chemical composition of the crustal rocks of the Earth and the composition of the ocean and the atmosphere are significant in evaluating sources of solutes in natural freshwater. The ways in which solutes are taken up or precipitated and the amounts present in solution are influenced by many environmental factors, especially climate, structure and position of rock strata, and biochemical effects associated with life cycles of plants and animals, both microscopic and macroscopic. -from Author
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Experiments were performed to demonstrate that saline interstitial waters under an arid coastal plain could be set in hydrodynamic movement to replace the evaporative loss near the surface. In contrast to movement in a vadose zone, which is related to capillary forces caused by surface tension, the type of movement we observed was induced by a vertical hydraulic gradient under the evaporated area. Fluid flow through porous media was induced by an upward decrease in hydrodynamic potential during evaporation. We propose to call this type of movement evaporative pumping. Experiments further verified that flow rate induced by evaporative pumping was directly governed by evaporation alone; linear flow rate through coarse sand and that through very fine silt was approximately the same under the same evaporative condition. Yet the movement apparently obeyed Darcy's law. Since the permeability of the medium was fixed, and the flow rate was dictated by evaporation, only the hydraulic gradient could be the dependent variable in the Darcy equation. We observed that the gradient was indeed much greater in relative impermeable silt than in permeable sand, when the water to replace evaporative loss must flow with the same rate through those media. Our experiments suggested that hydrodynamic movement induced by evaporation could be an effective mechanism to transport magnesium-bearing solutions through relatively impermeable sediments of an arid coastal plain. Computations showed that dolomitization by evaporative pumping could proceed at a rate to account for the origin of Recent dolomite crusts, and for the great thickness of ancient supratidal dolomites. In contrast, we believed that dolomitization by seepage reflux or by groundwaters cannot be extensive, because of the inadequate magnesium-supply rates by such waters.
Geological and hydrochemical aspects of Sawa Lake-S
  • A K Jamil
Jamil, A. K., 1977 :Geological and hydrochemical aspects of Sawa Lake-S. Iraq, Bull. Coll. Sci. Vol. 18, No. 1, pp. 221-253.
The physio -chimical Characteristic of Sawa Lake Water in Samawa City -Iraq
  • W F Hassan
Hassan, W.F., 2007: The physio -chimical Characteristic of Sawa Lake Water in Samawa City -Iraq. Marina Mesopotamica, 22, pp:167-179.
Hydrogeology and Hydrochemistry of Rehab area/South and South-West of Samawa city
  • A N Al-Shemari
Al-Shemari, A. N., 2006: Hydrogeology and Hydrochemistry of Rehab area/South and South-West of Samawa city. M.Sc. thesis, University of Baghdad, College of Science. 110p.
2012: A geomorphological study of dune fields and their environmental effects at Al-Muthana Governorate-Iraq
  • E A Abdul-Ameer
Abdul-Ameer, E.A., 2012: A geomorphological study of dune fields and their environmental effects at Al-Muthana Governorate-Iraq. D.Sc. thesis, University of Baghdad, College of Science. 163p.
Hydrogeological and hydrotechnical exploration in block 1, 2 and 3 (Southern Desert); final report on hydrogeology
  • N Al-Rawi
  • S Al-Sam
AL-Rawi, N., AL-Sam, S., and AL-Shavarka, L., 1983: Hydrogeological and hydrotechnical exploration in block 1, 2 and 3 (Southern Desert); final report on hydrogeology, hydrochemistry and water resources, Vol.9 SOM. Lib.204p.
The Source of Springs Water Oriented along the Faulted Zone of Southern Euphrates Rivers
  • A M Al-Shamma'a
Al-Shamma'a A.M., 2001 The Source of Springs Water Oriented along the Faulted Zone of Southern Euphrates Rivers, Proceeding of the7th Geological Jordan Conference, 27p
Geological Map of Iraq
  • V K Sissakian
Sissakian, V.K., 2000. Geological Map of Iraq. Scale 1: 1000 000, 3rd edit. GEOSURV, Baghdad, Iraq.
The influence of dissolved organic carbon, suspended particulates, and hydrology on the concentration, partitioning and variability psoriatic arthritis and concomitant fibromyalgia
  • M Shafer
  • J Overdier
  • J Hurley
  • D Armstrong
  • D Webb
Shafer, M. Overdier, J. Hurley, J. Armstrong, D. Webb, D. 1997: The influence of dissolved organic carbon, suspended particulates, and hydrology on the concentration, partitioning and variability psoriatic arthritis and concomitant fibromyalgia. IMAJ3, pp:147-150.
Sawa Lake: The Nature and Unique
  • S M Awadh
  • R E Muslim
Awadh, S. M. and Muslim, R. E., 2012: Sawa Lake: The Nature and Unique. Characteristics, Proceeding of the Second Scientific Symposium, Natural Heritage. Research Center and the Museum of Natural History, 82 Jun, 2006, Iraq, Baghdad.
Hydrogeological and hydrochemical sediment petrographical study of Sawa Lake
  • A Al-Naqash
Al-Naqash, A., B., 1977: Hydrogeological and hydrochemical sediment petrographical study of Sawa Lake, Bull. Coll. Sci. 18(1), pp:199-220.
Geochemistry and Mineralogy of the SamawaSaltern Southern Iraq
  • S Y Samaan
Samaan, S. Y., 1985: Geochemistry and Mineralogy of the SamawaSaltern Southern Iraq. M.Sc. thesis, University of Baghdad, College of Science. 183p. (In Arabic).
Hyrogeology of the Groundwater to the Al-Shanafiya Area/ South Iraq
  • S W H Al-Muqadi
Al-Muqadi, S. W. H., 2003: Hyrogeology of the Groundwater to the Al-Shanafiya Area/ South Iraq. M.Sc. Thesis, University of Baghdad.
Seawater Manual. Fundamentals of water chemistry for marine Aquarists
  • J M Edmund
  • Jr
Edmund, J.M. Jr., 2009: Seawater Manual. Fundamentals of water chemistry for marine Aquarists. Distributed by United Pet Group, Inc.
Oceans prentice-Hall printed by: SeaAgri, inc.Dunwaoody
  • K Turekiank
Turekiank.k., 1968: Oceans prentice-Hall printed by: SeaAgri, inc.Dunwaoody. GA30458.770-361-70
Hand book of hydrogeology
  • M E Altovisiki
Altovisiki, M. E., 1962: Hand book of hydrogeology. Geogoelitzet, Moscow, USSR (In Russian), 614p.
Saline water resource of North Dakota US Geol
  • C J Robinove
  • R H Longfort
  • J W Brook
Robinove, C.J., R.H. longfort and J.W. Brook., 1958: Saline water resource of North Dakota US Geol. Surv. Water Supply Paper 1428, pp:72.
Groundwater hydrology second edition
  • D K Todd
Todd, D. K., 2007: Groundwater hydrology second edition, John Wiley and Sous, Third Reprint. Inc. India. 535p.
A grows guide to water quality
  • C M Don
Don, C.M., 1995: A grows guide to water quality. University college station, Texas.
Climate data of recorded in Al-Sammwa station for period from
Iraqi Meteorological Organization., 2012: Climate data of recorded in Al-Sammwa station for period from (1990-2011).
  • Tamar Agha
Tamar Agha, M. Y., 1984. Final Report on Geology of the SouthernDesert, Block 1, 2 and 3, Vol. 3, GEOSURV Lib Baghdad
  • Tamar Agha
Tamar Agha, M. Y., 1984. Final Report on Geology of the SouthernDesert, Block 1, 2 and 3, Vol. 3, GEOSURV Lib Baghdad
  • T Buday
Buday, T., 1980: Stratigraphy and Paleogeography in Kassab, I. M. and Jassim, S. Z. (eds.).The Regional Geology of Iraq. Vol. 1, Geol. Surv.and Miner. Invest. Baghdad, Iraq, 445p.
Seawater Manual. Fundamentals of water chemistry for marine Aquarists. Distributed by United Pet Group
  • J M Edmund
Edmund, J.M. Jr., 2009: Seawater Manual. Fundamentals of water chemistry for marine Aquarists. Distributed by United Pet Group, Inc.