CAJ | 학술논문

得耳布尔铅锌矿位于森林沼泽景观.通过对低温富有机质环境中土壤元素的表生地球化学特征的研究表明,土壤中元素地球化学行为受到到基岩、土壤粒级、铁锰氧化物、有机质、酸性地表水的控制;残积层和腐殖层元素存在形式主要是铁锰氧化物态,铁锰氧化物对元素次生富集起到了很大的作用;有机质对元素的吸附作用受到土壤粒级、层位和有机质含量的影响.
득이포이연자광위우삼림소택경관.통과대저온부유궤질배경중토양원소적표생지구화학특정적연구표명,토양중원소지구화학행위수도도기암、토양립급、철맹양화물、유궤질、산성지표수적공제;잔적층화부식층원소존재형식주요시철맹양화물태,철맹양화물대원소차생부집기도료흔대적작용;유궤질대원소적흡부작용수도토양립급、층위화유궤질함량적영향.
The Deerbuer Pb-Zn deposit is located in a forest and swamp area. Element geochemistry of soil in the low temperature and rich organic matter environment was studied. It is shown that element geochemistry is influenced by rock, soil granularity, iron-manga-nese oxides, organic matter and acid precipitation, and that modes of occurrence of elements in eluvial and humus layers are mainly i-ron-manganese oxides which play a significant role in element enrichment. The adsorption of organic matter is affected by soil granulari-ty, horizon, and organic matter content.