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Rainy Days, Geographic Coordinates, Vitamin D, Silicon, Selenium and CHD in Finland in 1962-2014

Authors:
Volume 5- Issue 4: 2018
1/6
ISSN: 2574-1241
DOI: 10.26717/BJSTR.2018.10.001896
Töysa T.
Biomed J Sci & Tech Res
Research Article
Biomedical Journal of
Scientific & Technical Research (BJSTR)
Open Access
Introduction
Higher cardiac morbidity in eastern regions of Finland than
in the west, has been decades without satisfactory explanations
[1]. This east-west difference has been reported to have been
decreased by men from 1.36 to 1.26 in 1973-2002, but not by
women [2]. In period 1993-97 this risk ratio by men was still 1.33
[2]. High number of annual rainy days (RD) in East Finland has
been suggested to reduce vitamin D synthesis and affect on CHD
and general mortality [3]. In 1980 highly signicantly lower vitamin
D values have been reported from East Finland relative to South
Finland [4] (Table 2): [N cases; S-25(OH)D; standard deviation)]:

with 0.5 mcg vitamin D/100 g and fat spreads with 10 mcg/100

recommendation was doubled [5]. Dependence of S-25(OH)D on
moderate Mg and Se level is often passed [3]. The aim of this study
is to clarify CHD associations with Lat, Long, Alt, RD and Si.gw and
discuss the participating factors.
Material and Methods
Area units in this study are principally Finnish continental Rural
Centers (N 20) as follows: Provincial CHD mortality data of Finnish
middle-aged men in 1964-84 are from Valkonen and Martikainen
(1990) [6] as in [7,8]. Approximate male CHD data by Rural
Center (RC) - earlier Agricultural Advisory Centers - are attained
Rainy Days, Geographic Coordinates, Vitamin D,
Silicon, Selenium and CHD in Finland in 1962-2014
Töysä T*
Licentiate of Medicine, Specialty General Practice, Rehabilitation Hospital Vetrea Terveys Oy, Finland
Received: : September 25, 2018; published: : October 15, 2018
*Corresponding author: ysa T, Licentiate of Medicine, Specialty General Practice, Rehabilitation Hospital Vetrea Terveys Oy,
Pohjolankatu 15, FI-74100 Iisalmi, Finland
Abstract
Background: Higher cardiac as also general mortality in eastern regions of Finland than in the west, has been decades without satisfactory
explanation. High number of annual rainy days (RD) and lower serum vitamin D values has been associated with East Finland relative to South
Finland. Enrichment of dairy products was begun in 2002. In this study has been assessed regional CHD mortality (a sign of CHD morbidity) from
1964-84 [CHD. (64-84)] and CHD morbidity from 2012-14 [CHD. (12-14)], their association strength and stability with latitude (Lat), longitude
(Long), altitude (Alt), RD and groundwater silicon (Si.gw). Areal parts of Uusimaa were combined to one unit, as respectively by Varsinais-Suomi.
Number of area units was 18.
Results (R square %´s): [CHD. (64-84)]/ [CHD. (12-14)] associations: Long: 86/52.7%; RD: 61.3/44.2 %; Si.gw: 41.8/38.2 %; Alt: 33.5/32.3 %;
Lat 15.8/42.6 %. Alt explained best Si.gw (50.2 %). Long explained best RD. Changes in CHD associations were highest with Lat and Long, smallest

Conclusion:    
of RD in both periods and suggested on CHD association with serum vitamin D content. Anyhow decrease in CHD E/W ratio until period 2012-14

regulating factors, as Se, too. Changes in CHD E/W ratio during 1962-2002 associated with allowance or fertilization of Se. A new CHD risk factor Alt,

CHD mortality.
Keywords: CHD; Rainy Days; Latitude; Longitude; Altitude; Vitamin D; Silicon; Selenium; Solar Energy
Abbreviations: Alt: Altitude (Elevation Above Sea Level (m); CHD: Coronary Heart Disease; [CHD.(64-84)]: CHD Mortality in 1964-84; [CHD.(12-
14)]: CHD Morbidity by THL Index in 2012-14; Geographic Coordinates: Lat, Long and Alt; Lat: Nordic Latitude (°N); Long: Eastern Longitude (°E);
RC: Rural Center (Earlier Agricultural Advisory Center); RD: The (Regional) Number of Annual Rainy Days); Se: Selenium; Si: Silicon; THL: Terveyden
Ja Hyvinvoinnin Laitos-National Institute for Health and Welfare

Cite this article: Töysä T. Rainy Days, Geographic Coordinates, Vitamin D, Silicon, Selenium and CHD in Finland in 1962-2014. Biomed J
Sci&Tech Res 10(1)-2018. BJSTR. MS.ID.001896. DOI: 10.26717/ BJSTR.2018.10.001896. 2/6
Volume 10- Issue 1: 2018

of one province (N 17), in other cases (N 3) by weighting the CHD
values of different provinces by their cropland areas, which were
inside the RC in 1988 [7]. The data on cropland areas, as map and
label numbers (with one exception: Åland does not include in RC
04, continental RC 04 is labeled as 04.a.) are from [8] as in [7] and
calculated as follows:
a) CHD.Pirkanmaan=(26.5*CHD.Turku_and_Pori+75.1*CHD.
Häme)/101.6;
b) CHD.Itä-Hämeen=(41.5*CHD.Häme+15.9*CHD.
Mikkeli+7.6*CHD.Central_Finland)/65.0;
CHD. Keski-Pohjanmaan = (45.7*CHD.Vaasa+23.7* CHD.
     
[9] included errors, because they were aimed for [10] with some
combined RC´s). Regional CHD morbidity indices in 2012-14
[CHD. (12-14)] from National Institute for Health and Welfare [11]
       
(Lat) (Figures 1 & 2) and longitude (Long) (Figure 3) of each RC
have been determined by their central commune [12]. Alt was got
via internet search: Name of central commune and “geographic
coordinates” or “elevation above sea level”. Map of annual rainy
days from Finnish Meteorological Institute [13] was combined
with the map of RC´s [8], similar with the map of Finnish Regions
[12]. Then approximate mean RD by RC was visually approximated
(in Lapland by the central commune) (Figure 1). Thereafter Parts
Uusimaa (RC 01 and and 02) and respectively parts of Varsinais-
Suomi (03, 04.a) were combined by weighting values by the part-
areas (Table 1).
Table 1: Rural centers with central communes, male CHD mortality in 1964-84, THL.CHD.index, Latitude, Longitude and annual
rainy days in 1981-2010, Altitude and groundwater silicon.
Regions (Rural Centers) Central Commune CHD. (1964-84) CHD. (2012-14) Latitude Longitude Altitude Rainy Days Si.gw
1/100,000 THL.index 0N0E m d/a mEq/L
Uusimaa (01;02) Järvenpää;Espoo 447 78.0 60.4 24.9 39 182 1.12
Varsinais-Suomi (03;04.a) Aura;Nagu/Nauvo 386 87.4 60.6 22.5 48 170 1.12
05 Satakunnan Noormarkku 386 91.4 61.6 21.9 44 165 0.98
06 Pirkanmaan Ylöjärvi 407 92.4 61.6 23.6 107 181 0.93
07 Hämeen Renko 414 89.1 60.9 24.3 107 190 1.12
08 Itä-Hämeen Asikkala 454 106.2 61.2 25.5 74 186 0.98
09 Kymenlaakson Anjalankoski 511 97.0 60.7 26.8 18 195 1.14
10 Etelä-Karjalan Jouseno 511 129.8 61.1 28.5 80 200 0.93
11 Mikkelin Juva 531 124.9 61.9 27.9 98 195 0.91
12 Kuopion Maaninka 564 135.5 63.2 27.3 88 200 0.78
13 Pohjois-Karjalan Kontiolahti 622 122.9 62.8 29.8 138 195 0.81
14 Keski-Suomen Saarijärvi 515 106.0 62.7 25.3 140 190 0.90
15 Etelä-Pohjanmaan Nurmo 370 100.6 62.8 22.9 47 183 1.07
16 Österbottens Svenska Mustasaari 370 98.3 63.1 21.7 15 160 1.78
17 Keski-Pohjanmaan Toholampi 432 117.6 63.8 24.3 94 173 0.90
18 Oulun Ylikiiminki 553 121.8 65.1 26.4 85 185 0.85
19 Kainuun Ristijärvi 553 141.0 64.5 28.2 160 210 0.65
20 Lapin Rovaniemi 529 127.8 66.5 25.7 92 195 0.70
04.b Åland Maarianhamina 265 98.6 60.2 19.9 11 165 0.68
 Volume 10- Issue 1: 2018
Cite this article: Töysä T. Rainy Days, Geographic Coordinates, Vitamin D, Silicon, Selenium and CHD in Finland in 1962-2014. Biomed J
Sci&Tech Res 10(1)-2018. BJSTR. MS.ID.001896. DOI: 10.26717/ BJSTR.2018.10.001896. 3/6
Figure 1: Finnish map with Rural Centers and their approximate
number of rainy days (in the east the darkening gray is a sign of
higher number of rainy days, opposite in the west.
Figure 2: Association of latitude (Lat) with CHD in two periods.
Figure 3: Association of longitude (Long) with CHD in two pe-
riods.
Figure 4: Association of altitude (Alt) with CHD in two periods.
Discussion
This study showed CHD stability in different decades and

association. Most soil and groundwater factors and temperature
were associated nearer to south-north axis [1,7,9,10,12]. RD
“explained” CHD stronger before (66.8%) than after (43.8%)
     
annual solar energy in Finland on an average 35% compared with
cloudless sky [15]. So it can be expected that RD, a surrogate of
 
status of humans [3,4]. Anyhow after declining, CHD-Long factor
remained as the strongest environmental CHD factor during the
last period. Old school books wrote that rains are associated with
          


Cite this article: Töysä T. Rainy Days, Geographic Coordinates, Vitamin D, Silicon, Selenium and CHD in Finland in 1962-2014. Biomed J
Sci&Tech Res 10(1)-2018. BJSTR. MS.ID.001896. DOI: 10.26717/ BJSTR.2018.10.001896. 4/6
Volume 10- Issue 1: 2018

Long and RD were remarkably reduced between the periods, RD-
CHD association ad 44.2, which is about the same as Si.gw-CHD
association (38.2%) (Table 2). I.e. as during reduction of East
factors (i.a. vitamin D) Alt factors (i.a. Si.gw) (Figure 6) remained

losses) outwards. So it can be understood that weathering, erosion,
       
with CHD’s makes Alt a new CHD risk factor. Alt explained best
Si.gw by 50.2 % (Table 3).
Figure 5: Association of annual rainy days (RD) with CHD in
two periods
Figure 6: Association of ground water silicon (si.gw) with CHD
in two periods.
Table 2: Inter-regional associations between age adjusted CHD mortality of middle-aged men 1964-84, THL CHD morbidity index
2012-14 and environmental factors.
CHD.M.(1964-84) CHD.(2012-14) Latitude Altitude Longitude Rainy Days Si.gw
100*(R Square)
CHD.M.(1964-84) 56.2 15.8 33.5 86.0 61.3 41.8
CHD.(2012-14) 56.2 32.3 52.7 44.2 38.2
Latitude 15.8 42.6 14.2 3.2 4.1 16.0
Altitude 33.5 32.3 14.2 30.8 36.1 50.2
Longitude 86.0 52.7 3.2 30.8 74.7 36.4
Rainy days 61.3 44.2 4.1 36.1 45.4
Si.gw 41.8 38.2 16.0 50.2 45.4
Table 3.
Significance levels (N = 18)
 21.8  *
 34.0  **
 48.0  ***
East-west CHD mortality ratio (CHD E/W) (Figure 8) was
additionally assessed by male CHD data (3-year means) from
1962-86 [6] and Pajunen et al. [2] from 1973-2002. E/W ratio was
 
because of missing data. Then this ratio was adjusted to human
values [2] by subtracting 0.014 from it: E/W ratio was in 1962-
68 1.30, 1968 it increased to 1.35 and its 5-year means stayed
above 1.33 until 1998. 1968 was associated with reduction of
imported Se-rich grain [16]. After period 1978-82 it declined from
level 1.37 to 1.34 associated with the beginning of Se fertilization
[17,18]. The decreased to 1.26 after 1997 associated with the
second increase of Se-fertilization (for non-cereals) [18]. The
unexpectedly high difference in S-25(OH)D [4] between south and
east was obviously not dependent only on vitamin D intake per os
and per skin, but on proactive and counteractive factors, e.g. Mg,
Se [3] and obviously Si [19,20]. Weight of vitamin D as a CHD. East
factor seems to be much weaker than expected [3]. Silicon content
of food was obviously decreasing in the 1960´s with increasing
total fertilization and increasing with decrease of total fertilization
(after 1989), but changes were not as abrupt as in CHD E/W ratio.
 Volume 10- Issue 1: 2018
Cite this article: Töysä T. Rainy Days, Geographic Coordinates, Vitamin D, Silicon, Selenium and CHD in Finland in 1962-2014. Biomed J
Sci&Tech Res 10(1)-2018. BJSTR. MS.ID.001896. DOI: 10.26717/ BJSTR.2018.10.001896. 5/6
Comparing of mortality statistics with morbidity indices includes
several problems/biases, which are passed in the assessment above
because of their complexity. Data has been treated as if they came
from the same data base. Interesting observetions: The moderate
high CHD in Uusimaa provice (RS´s 01 & 02) in 1964-84 could be
dependent on migration, lower synthesis of vitamin D (high houses,
indoor work), it is suspicious that vitamin D alone could explain it.
Causes for CHD reduction before 2014 in Uusimaa could be based
i.a. on higher vitamin D supply and possible validity problems with
THL CHD index (big private sector – part of the use of private sector
can stay out of study statistics). High CHD mortality of Kymenlaakso
(RC 09) in 1964-84 together with good soil parameters [9] and
its recovery until 2014 is in harmony with RD action in 1964-84
        
risk factor(s) [20] seem(s) to deserve attention and research
work. In this chapter associations are calculated after exclusion
of Åland with low and obviously misleading Si.gw values [1]. Even
preliminary data from this summer suggest that Si content of milk
from Åland (with low Si.gw and high Ca/Mg ratio in soil and gw)
could be the higher than in continental Finland (Figure 7).
Figure 7: Association of CHD from two period with each other.
Figure 8.
Conclusion
CHD morbidity showed high inter-regional stability between
 
of RD in both periods and suggested on CHD association with
serum vitamin D content. Anyhow decrease in CHD E/W ratio until

Serum vitamin D [S-25(OH)D] indicates not only allowance (per os
& per skin) of vitamin D, but regulating factors, as Se, too. Changes
in CHD E/W ratio during 1962-2002 associated with allowance or
fertilization of Se. A new CHD risk factor Alt, with high association
with Si.gw is presented. Calculated conclusions are based on
       
CHD mortality.
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Cite this article: Töysä T. Rainy Days, Geographic Coordinates, Vitamin D, Silicon, Selenium and CHD in Finland in 1962-2014. Biomed J
Sci&Tech Res 10(1)-2018. BJSTR. MS.ID.001896. DOI: 10.26717/ BJSTR.2018.10.001896. 6/6
Volume 10- Issue 1: 2018
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ISSN: 2574-1241
DOI: 10.26717/BJSTR.2018.10.001896
Töysa T. Biomed J Sci & Tech Res
... Uudenmaan' and its southern RC '(02). Nylands Svenska' are combined to Uusimaa as in [11] responding together rather accurately combined Uusimaa of [12]. ...
... Varsinais-Suomen' and RC '(04.a) mainland Finska Hushållningss.' are combined to Varsinais-Suomi, which is a Finnish region as such, as in [11]. ...
... (=Ostrobothnia) was excluded because of small number of samples (11) and exceptionally high Si.gw.mean/Si.gw.median ratio 1.62 (1.78/1.10) [7]: On an average this ratio in RC´s was 1.08 (+/-0.14) ...
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ISSN: 2574 -1241 DOI: 10.26717/BJSTR.2019.20.003450 Regional K buffer in organic and mineral soils and their associations with estimated cation exchange capacity, pH, groundwater silicon and some environmental factors in continental Finland 1986-90 with discussion on inorganic carbon Töysä T* Licentiate of Medicine, Specialty General Practice, Rehabilitation Hospital, Finland *Corresponding author: Töysä T, Licentiate of Medicine, Specialty General Practice, Rehabilitation Hospital, Finland Received: July 25, 2019 Published: August 09, 2019 Citation: Töysä T. Regional K buffer in organic and mineral soils and their associations with estimated cation ex¬change capacity, pH, groundwater sil¬icon and some environmental factors in continental Finland 1986-90 with discussion on inorganic carbon. Biomed J Sci & Tech Res 20(3)-2019. BJSTR. MS.ID.003450. Keywords: K buffer; CEC; Silicon; pH; Organic Soils; Mineral Soils; Groundwa¬ter; Geographic Factors Abstract Cation exchange capacity (CEC) is the total capacity of a soil to hold exchangeable cations. It influences the soil’s ability to hold onto essential nutrients and provides a buffer against soil acidification. Organic matter has a very high CEC. Anyhow potassium buffer power is known to be weak in other than clayey and silt soils, especially in peat, why fertilization can cause excessive variation in plant mineral composition. Finnish soil samples are collected mainly in autumns. That’s why they obviously reflect K buffer power of organic soils, too. The aim of this study is to clarify regional associations of cropland K, (estimate) CEC (Ca+Mg+K) and pH, in organic (org) and mineral soils (min), groundwater (gw) silicon (Si) and geographic factors Latitude (Lat) and Longitude (Long). The data are from old sources. Results: Mean regional (CEC.org/CEC.min) ratio [CEC. (org/min)] was 1.28, mean K.(org/min) inversely 0.63 and pH. (org/min) 0.91. K.org was stronger explained by CEC. min (91.8 %), by Si.gw (71.0 %) and by [Lat; Long] (67.4 %) than by CEC.org (63.6 %), by pH.org (56.9 %) or by pH. min (43.0 %). Associations between single parameters were significant and positive. Si.gw explained better K.org than K.min and pH.org stronger than pH.min. Si.gw explained positively K.(org/min) (55.7 %, p = 0.001) and negatively CEC. (org/min) (32.0 %, p = 0.018). Conclusion: In continental Finland regional Si.gw – obviously associated with weathering rate - explained significantly variation in K.org, K.min, K buffer, CEC.org, CEC.min, pH.org, pH.min, K.(org/min) and CEC. (org/min). Association of Si.gw with soil inorganic carbon is discussed. PS Feb 17, 2020: In continental Finland regional groundwater Si – a metabolite in carbonate silicate cycle, a sign of carbon sequestration, possibly a useful measure of weathering rate - explained significantly variation in autumnal K.org, K.min, CEC.org, CEC.min, pH.org, pH.min, K.(org/min) and CEC.(org/min). Groundwater Si obviously reflected the cropland Si, which increased K-buffer capacity and reduced K-leakage especially in organic soils.
... Latitude is associated with shorter pasture period and shorter period to get fresh grass and with less effective weathering (temperature dependent). Longitude is associated with soil age: period open for weathering and erosion (erosion = weathering + transport), additionally associated with altitude and higher number of rainy days [25] and so obviously with lower level in vitamin D synthesis in the skin. ...
... Explanation for rainy days is the higher altitude in the eastern regions [25]. Earth elevation in the western Finland has been ca 250 m during the last 9,000 yrs [26]. ...
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Silicon as an antioxidant. Groundwater (gw) Ca as such is an indicator of gw hardness and possible an indicator of plant silicon (although additional studies are needed). Environmental factors affect strongly on plant silicon, but it is suggested that long-term changes in plant silicon indicate changes in (crop)land carbon binding and changes in water holding capacity
... Although this weighting system is disputable, it is not treated in Discussion. Data on provincial CHD mortality of men processed in[4] and their adjustments for RC's is represented in[22]. Approximate province figures for period 1974-83 are attained fromTable 1in[4] by weighting the values of the last three columns by 1, 2 and 2 (Table 4). ...
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Biomedical Journal of Scientific and Technical Research Research Article ISSN: 2574 -1241 D_O_I_:_ _1_0_._2_6_7_1_7_/_B_J_S_T_R_._2_0_2_0_._2_6_._0_0_4_4_2_8_ _ Regional Groundwater Si and Mg/Ca, Soil Mg/Ca, Soil-Types, Cardiac Diseases and Local Long-Term Dolomite Application - Soil Values from Two Periods Suggest on Different Roles of Mg and Si in Cardiac Epidemiology Töysä T* Rehabilitation Hospital Vetrea Terveys Oy, Finland *Corresponding author Article info: Received March 13, 2020 Published April 08, 2020 Abstract Objective: For decades has been discussed on cardio-protective factors associated with drinking water, Si, Mg, etc. This study is assessing Finnish regional cropland Mg/ Ca values (by total, “tot” and 6 separate soil types) from periods 1966-70 (“68”) and 1986-90 (“88”), soil-type proportions (Prp) of mineral soils (min), e.g. moraines (mor) and sands, groundwater (gw) Si and (Mg/Ca), male (M) CHD mortality, ratios of human CHD and other cardiac mortality to total mortality [(CHD/Tot) and (Card.o/Tot)] in 19 regions. Preferring Si.gw median (Si.gw.md) to Si.gw.mean is explained. Results: Finland could be divided into 4 different areas: Åland (carbonate soils), SW, SE and North (5 regions with long-term dolomite application). In both periods (Mg/Ca), with exception of sandy clay, was highest in the North, lowest in Åland and associated inversely with coarseness of soil-type. After exclusion of North: [(Mg/Ca).soil.68] was explained 87.2 % by [(Mg/Ca).gw] (in whole country only by 27.7 %, p = 0.021), by Si.gw.md 71.7 % (p < 0.001). In continental Finland (on non-carbonate soils): Si.gw.md was explained inversely: 48.4 % (p=0.007) by Prp. {[mor/(mor+sands)]; [(mor+sands)/ min)]}.88, 53.5 % (p = 0.001) by [M.CHD.(74-83)], 54.6 % (p < 0.001), by [(CHD/Tot). (87-04)]; positively 39.2 % (p = 0.005) by [(Mg_Ca).gw]. In whole country [(Card.o/ Tot). (1987-2004)] was explained inversely by [(CHD/Tot).(87-04)], better by more coincidental [(Mg/Ca).tot.88], (45.2 %, p = 0.002) than by [(Mg/Ca).tot.68] (40.9 %). Conclusion: CHD and [(CHD/Tot)] mortality associated stronger with parameters of soil weathering ability, indicated by soil-type distribution, groundwater Si and (Mg/ Ca). (Card.o/Tot) associated stronger with cropland (Mg/Ca) and was affected by long-term dolomite application. PS May 4, 2020: The author was thinking for more than one year, why milk silicon during pasture period in 2018 was 10-100-fold to earlier studies. Explanation was acid-soluble contra water-soluble silicon as explained here. (but definition of water-soluble silicon in solid material as grain is anyhow impossible!). In April 2020 the first analyses of acid-soluble Si in milk during indoor feeding were 2-3 ppm (1/100 from the highest earlier values). Studies continue. Possible explanation: earth eating during pasture. Citation (Xin Wang, Weihong Li, Haoxin Tong. A Comparative Study of TransE and TransH Algorithms in Spatial Address Representation Learning. Biomed J Sci & Tech Res 26(5)-2020. BJSTR. MS.ID.004428.) is a lapsus
... In combined regression by [Temp; pH.soil] pH coefficient got negative value for Si.gw [5]. Åland has been excluded from this survey because the availability of Si seems not to be associated with Si.gw [4,6]. Groundwater pH is different in immediate analysis on the field (pH.gw.field) to the laboratory survey (pH.gw.lab). ...
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Regional pH in five Agricultural Soil-types – Associations with Temperature and Groundwater Si in Continental Finland Töysä T Licentiate of Medicine, Specialty General Practice, Rehabilitation Hospital VetreaTerveys Oy *Corresponding author: Töysa T, Rehabilitation Hospital VetreaTerveys Oy, Pohjolankatu 15, FI-74100 Iisalmi, Finland. Email: timo.toysa@fimnet.fi Abstract The role of weathering in carbon sequestration has not got attention enough. This study is assessing regional factors: annual temperature (Temp), groundwater (gw) Si, agricultural total (tot) and soil-type pH´s and soil-type proportions (Prp) of moraine (mor), sand, silt, clay and mull soils in order to clarify whether weathering could be associated with pH variation in different soil-types. [mor + sand soils are labeled as coarse mineral soils (coms), respectively coms + silt + clays as mineral soils (miner). 1 – Prp.miner = Prp organic (org). Moraines, sands and clays include several subclasses]. Materials and methods: Regional soil pH´s, soil-type Prp´s, Si.gw and Temp are from old sources. N of regions in statistical survey was 15 (after combining 2 and excluding 4 of them – Åland + 3 continental regions - because of carbonate soil prominence or statistical inadequacy). N of soil-samples was ca 570,000 and gw samples 596. Results: Regional pH´s ranged from 5.35 to 6.20 in different soil-types. Temp associated significantly positively with pH´s, Si.gw and Prp.miner. Si.gw-pH associations [(Pearson/Spearman): pH.mor (+0.42/+0.37), pH.sands and silts [(+0.53, +0.52)/(+0.58, +0.55)], pH.clays (+0.74/+0.77)] seemed to increase from coarse towards finer mineral soils. Represented soil-type pH´s associated significantly with pH.tot. Conclusions: Regional pH.mor, pH.sands, pH.silt and pH.clays associated significantly with pH.tot and Temp. pH associations with Si.gw seemed to increase towards finer mineral soils. Regional Prp.org, a measure of soil ageing, associated negatively with pH´s.
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Regional Groundwater Hardness and Silicon, Cropland Fertility and CHD in Finland Timo Töysä*1 1Specialty General Practice, Rehabilitation Hospital Vetrea, Finland Received: December 17, 2017; Refer: BJSTR-MS.ID.000623 Pohjolankatu 15, FI-74100 Iisalmi; Email: timo.toysa@fimnet.fi Abstract The status of silicon (Si) in agriculture, veterinary and human medicine is not clear. This survey is based on old data, but groundwater (from springs and dugwells) data have been newly classified by 21 Rural Centers (RC). RC CHD has been estimated by provincial data. The aim of this paper is to clarify associations between CHD mortality, groundwater (GW) hardness (Ca+Mg), Si.gw, cropland (soil) (Ca+Mg) – a measure of soil fertility - and, pH and temperature (Temp) with regional parameters [latitude (Lat), longitude (Long)]. Regressions are given separately for the whole Finland (“21.RC”) and continental Finland (“20.RC”), i.e. without Åland – the only RC with pH.soil > 6.2. Directions of trend lines of variables have been approximated. Results: CHD regressions by Si.gw, by (Ca+Mg).gw and by (combined) [Lat;Long], (Ca+Mg).gw regressions by (Ca+Mg).soil and by [Lat;Long] and, Si.gw regressions by (Ca+Mg).gw, by [Lat;Long], by [Temp;(Ca+Mg).soil] and by [Temp;pH.soil] have been computed. In RC.20 all associations were significant (p < 0.018). In RC.21 all regressions without Si.gw were stronger than in RC.20, but by including Si.gw associations were weaker with one exception: [Temp;pH.soil] explained Si.gw stronger than in RC.20 (by 68 %). The approximated CHD trend line angle was smaller than the respective angles of Si.gw and (Ca+Mg). Conclusion: In RC.20, where soil pH was below 6.2, Si.gw and (Ca+Mg).gw were highly positively inter-correlated and soil fertility could be predicted by regional Si.gw. In RC.20 regression by Si.gw explained better CHD than by (Ca+Mg).gw. Supposedly the health effects of Si could be mediated directly through (soluble) Si in soil and via factors associated with (Ca+Mg). In regional gw analyses the effect of (mother earth) pH needs attention.
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Soil pH, Ca and Mg Stability and pH Association with Temperature and Groundwater Silicon Timo Töysä*1 and Osmo Hänninen2 1Specialty General Practice, Rehabilitation Hospital Vetrea, Finland 2Department of Physiology, University of Eastern Finland, Finland Received: November 16, 2017; Published: December 04, 2017 *Corresponding author: Timo Töysä, Specialty General Practice, Rehabilitation Hospital Vetrea, Pohjolankatu 15, FI-74100 Iisalmi; Soil pH, Ca and Mg Stability and pH Association with Temperature and Groundwater Silicon Timo Töysä*1 and Osmo Hänninen2 1Specialty General Practice, Rehabilitation Hospital Vetrea, Finland 2Department of Physiology, University of Eastern Finland, Finland Received: November 16, 2017; Published: December 04, 2017 Abstract It is generally known that pH, Ca and Mg have changed remarkably during 1961-90, but their inter-areal variation seems not have been fully discussed nor explained. Parameters of cropland have been earlier associated with CHD mortality. Silicon (Si) and temperature (Temp) have been earlier assessed with human CHD mortality. In this study we have assessed soil values of 21 Rural Centers (RC) from the 1960's, 1970's and 1980's, [(60's) (70's), (80's)] with respective mean annual temperatures from 1981-2010 and mean groundwater (gw) Si content. Results: Combined regression by pH.(60’s) and pH.(70’s) explained pH.(80) by 96.8 % (p < 0.001). Ca.(60’s) and Ca.(70’s) explained respectively Ca.(80’s) by 99.3 % (p < 0.001) and Mg.(60’s) and Mg.(70’s) explained respectively Mg.(80’s) by 92.3 % (p < 0.001). Combined regression by Temp and Si explained pH.(80’s) by 86.5 % (p < 0.001). Respectively combined regression by Temp and pH.(80’s) explained gw Si by 77.5 % (p < 0.001). Conclusion: Groundwater silicon is associated with the soil matrix factor (sources of groundwater silicon/silicon colloids?), which seems with temperature to explain inter-areal pH variation and obviously is associated with relative local stability of cropland Ca and Mg (and soil fertility). Maybe now is the time to increase Si trials in agriculture.
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Background Due to vitamin D intake below recommendation (10 µg/day) and low (<50 nmol/l) serum 25-hydroxycholecalciferol (25(OH)D) concentration in Finnish population, the fortification of liquid dairy products with 0.5 µg vitamin D/100 g and fat spreads with 10 µg/100 g started in Finland in December 2002. In 2010, the fortification recommendation was doubled. The aim of this study was to investigate whether the vitamin D intake and status have improved among Finnish adults as a consequence of these nutrition policy actions. A further aim was to study the impact of vitamin supplement use to the total vitamin D intake. Methods A cross-sectional survey was conducted every 5 years. The National FINDIET Survey was conducted in Finland as part of the National FINRISK health monitoring study. Dietary data were collected by using a computer-assisted 48-h dietary recall. In 2002, dietary data comprised 2007, in 2007, 1575 and 2012, 1295 working aged (25–64 years) Finns. Results The mean D-vitamin intake increased from 5 µg/day to 17 µg/day in men and from 3 µg/day to 18 µg/day in women from 2002 to 2012. The most important food sources of vitamin D were milk products, fat spreads and fish dishes. The share of milk products was 39% among younger men and 38% among younger women, and 29% among older men and 28% among older women. Fat spreads covered on average 28% of vitamin D intake, except for younger men for which it covered 23%. Fish dishes provided 28% of vitamin D intake for older men and women, and approximately 18% for younger ones. In January–April 2012, the average serum 25-hydroxycholecalciferol (25(OH)D) concentration for men was 63 nmol/l for men and for women 67 nmol/l for women. Conclusions The fortification of commonly used foods with vitamin D and vitamin D supplementation seems to be an efficient way to increase the vitamin D intake and the vitamin D status in the adult population.
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Agro-Geology and CHD in Finland
  • T Toysa
  • O Hanninen
Toysa T, Hanninen O (2015) Agro-Geology and CHD in Finland. JJ Agriculture 1(2): 006.
The eastern and western differences in coronary heart disease were reduced in men over 30 years of follow-up
  • P Pajunen
  • J Torppa
  • M Huohvanainen
  • V Salomaa
  • E Vartiainen
Pajunen P, Torppa J, Huohvanainen M, Salomaa V, Vartiainen E (2013) The eastern and western differences in coronary heart disease were reduced in men over 30 years of follow-up. Finnish Medical Journal 59: 16.