Extensive excavation of mangrove soils for aquaqulture ponds without correct knowledge and technique leads to the disturbance of acid sulfate soils (ASS) due to exposure of iron sulfide to air. This condition has been recorded in many places, particularly in southeast Asia, where the disturbance of ASS generates numerous environmental problems, such as: poor soil and water quality, reduction of aquaculture The study used three replications in subsurface soils near roots, and in the surface layer for some variables. The variables examined include pH, pHfox, redox potential, Titratable Actual Acidity (TAA), Titratable Potential Acidity (TPA), Titratable Sulfidic Acidity (TSA), water-soluble sulfate, HCl extractable sulfur (SHCl) or KCl extractable sulfur (SKCl), Peroxide Sulfur (SP), Peroxide oxidisable sulfur (SPOS), pyrite, organic content, grain size, total metal and metal fractionation. The density, establishment and the growth of Rhizophoraceae were also determined.
Both the experimental and field study demonstrated that the general geochemical condition required by mangrove seedlings are: higher pH and pHfox, and a reducing environment. Compared to the existing acidity (TAA) and other associated properties that count for the existing acidity level, such as water-soluble sulfate, extractable sulfur, exchangeable Al and Fe, the amount of potential acid (TPA and TSA) and pyrite on surface soils strongly correlated with the acidity, density, establishment and growth of the seedlings in the field study area. Higher amounts of potential acidity, including pyrite in surface soils, provided higher opportunities to oxidise in oxidative environments, which then release water-soluble sulfate, extractable sulfur, and exchangeable Al into subsurface soils, decrease pH and pHfox, and affect the density, establishment and growth of mangrove seedlings in the field study area.
The experimental study showed that the number of seedlings survived in non-ASS environment was higher compared to that in ASS environments. Lower sulfate and total extractable sulfur provided a good environment for mangrove seedlings to live under the non-ASS experimental environments. However, measured sulfur species as a single factor did not directly affect the density, establishment and growth of the seedlings in the field area. Sulfide correlates negatively to the establishment and growth of the seedlings. The type of environments (non-ASS and ASS) did not significantly affect the values of either the seedlings‘ total fresh length or their root length in the experiment at work. Mangrove seedlings can still grow and survive in high acidity but with lower values of density, establishment, and relative growth rate.
The concentration of metals in the environment influenced the concentration of metals in root tissues of Rhizophora stylosa seedlings. However, increasing concentration of metals (Fe, Al, Ni and Cu due to ASS disturbance in both experiment and field studies as well as addition of Ni and Cu in the experimental study did not increase BCF values. The selective mechanisms production, death of vegetation and aquatic life, and more.
ASS is a stress factor that is responsible for the failure of some mangrove restoration projects. However, there is evidence that natural revegetation of mangroves has occurred in some abandoned ponds. Available published papers on the geochemical factors that affect the success or failure of rehabilitation in ASS areas are very few, and this makes it difficult to achieve successful rehabilitation. Geochemical studies of mangrove rehabilitation in ASS environments are essential, since different areas may have different geochemical conditions. Additionally, the interactions among geochemical factors in ASS environments are complex and can affect the response of mangrove seedlings.
The establishment of mangrove seedlings in ASS environments would deal with several potential problems, particularly acid conditions and high concentration of metals. This research focuses on the concentration of two major elements released in ASS environments aluminium (Al) and iron (Fe), and two mobile metals under ASS conditions nickel (Ni) and copper (Cu).
The main objective of this study is to evaluate various geochemical factors involved in ASS environments, which in turn influence the response of mangrove seedlings to ASS. This study also seeks to determine the accumulation and translocation of metals within mangrove seedling tissues in relation to the concentration of metals in the soils of various environments, and their relationship to the mangrove seedlings‘ establishment and growth.
To achieve these objectives, a laboratory study was conducted at the Aquaculture Laboratory at QUT. For comparison, a field study was conducted in abandoned aquaculture ponds situated in the Mare District, adjacent to the Gulf of Bone, South Sulawesi, Indonesia. The study species in the laboratorory trials was Rhizophora stylosa, and the species examined in the field study included mainly R. stylosa and R. mucronata.are clearly shown in this study, where the seedlings tended to accumulate metals to certain amount based on their function and limited adsorption of non-essential metals. In regards to high levels of metals, mangrove seedlings regulated, retained metals mainly in their roots and employed an exclusion strategy, distributed them to aerial parts with low mobility and excreted them through leaf tissues.
The amount of potential acid (TPA and TSA) and pyrite in the surface soils strongly correlated with the acidity, density, establishment and growth of the seedlings. The presence of pyrite in surface soils allowed oxidation process to occur, which then enhanced the release of water-soluble sulfate, extractable sulfur, and exchangeable Al to subsurface soils, thus influencing the density and growth of mangrove seedlings. In contrast, the existing acidity (TAA) of both surface and subsurface soils, and associated existing acidity (water-soluble sulfate, extractable sulfur, exchangeable Al and Fe) in subsurface soils did not directly control the density, establishment and growth of the mangrove seedlings in the field study area. Exchangeable Al had a negative correlation with the establishment of the seedlings.
The free inundation of seawater produced an improvement in the soil quality of the study area, including higher pH (field and oxidisable), and low organic content. Free tidal inundation also generated low existing acidity, potential acidity and pyrite percentage on surface soils and reducing environments, therefore reducing the opportunity for pyrite to oxidise. Accordingly, the amounts of water-soluble sulfate, extractable sulfur and exchangeable Fe and Al on subsurface soils were low. Low organic material in these sites caused a low amount of SP and SPOS. Furthermore, physical and geochemical factors, such as: pH, redox potential, grain size, sulfur species affected metal concentrations in both soils and roots. All these processes highlight the importance of tidal inundation in improving soil quality and providing a good environment, which results in higher density, establishment and relative growth of mangrove seedlings in mangrove restoration projects. Good water circulation also allows propagule supply, therefore enabling mangroves to establish naturally.
This study provides a better understanding of the response of mangrove seedlings under conditions of various ASS, high metal concentrations, and non-ASS environments, as well as a recommended best strategy for achieving successful restoration in similar conditions.