Manganese and Sulfur Reduction by Soil Fungi on Post-Coal Mining Areas at Kutai Kartanegara, East Kalimantan

B. Widhayasa, Sudrajat Sudrajat, Rusdiansyah Rusdiansyah
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Abstract

At such levels, manganese and sulfur can damage ecosystems and water distribution systems and causes serious problems to surrounding water-soil bodies in the post-coal mining areas. Soil fungal has a positive contribution to the improvement of soil physical and chemical properties. This research aims to determine the population size and diversity of soil fungi related to the manganese and sulfur concentrations at various stages of reclamation in East Kalimantan. The numbers of soil fungi increased in the year after reclamation and then decreased after aging for nine years. Aspergillus, Penicillium, Cephalosporium, Gliocladium, Humicola, Trichoderma, and Paecilomyces, were among the fungi found colonizing in the soil of the reclamation areas. The numbers of soil fungi were found negatively correlated with manganese concentrations. A negative correlation found between the numbers of soil fungi and sulfur concentrations. The slightly higher number of soil fungi in the reclamation areas can be attributed to lower manganese and sulfur concentrations.
东加里曼丹Kutai Kartanegara采煤后土壤真菌对锰和硫的还原作用
在这样的水平下,锰和硫会破坏生态系统和水分配系统,并对采煤后地区周围的水土体造成严重问题。土壤真菌对土壤理化性质的改善有积极的贡献。本研究旨在确定东加里曼丹不同开垦阶段与锰和硫浓度相关的土壤真菌的种群规模和多样性。土壤真菌数量在垦殖后1年内呈上升趋势,9年后呈下降趋势。在垦区土壤中发现了曲霉、青霉菌、头孢菌、胶质菌、Humicola、木霉和拟青霉等真菌。土壤真菌数量与锰浓度呈负相关。土壤真菌数量与硫浓度呈负相关。复垦区土壤真菌数量略高可归因于较低的锰和硫浓度。
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