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A Study of Influence of Marsh Wetland Reclamation and Cultivation on the Features of Metallic Elements Distribution

机译:沼泽湿地回收和培养对金属元素分布特征的影响研究

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Through gauging the contents of pH,SOM,and metallic elements such as,A1,Fe,Hg,Pb,Cu,and Mn in the soft of typical Deyeuxia angustifolia wetland,corn fields and rice fields on the Sanjiang Plain,using the approach of space as a substitute for time,this paper discusses the contents of metallic elements and changes in the features of their profile distribution after the wetland is developed as farmland.The results showed that after the wetland was developed as farmland,the SOM content in soil would be lowered,with pH impacted significantly.The SOM content was positively correlated with Fe only,while the pH was positively or negatively correlated with most metallic elements in soil.After the wetland was reclaimed as paddy field,pH in soil rose,while A1,Fe,and Pb was enriched,and Mn was lost; after it was reclaimed as dry farmland,pH in soil lowered,while A1,Fe,and Pb were lost,and Mn was enriched.Hg was lost in both dry farmland and paddy field,while the changes in Cu were significant.The wetland reclamation and cultivation led to the change in pH conditions,which might be the main factors causing the changes in the content of soil metallic elements and features of their profile distribution.
机译:通过计量pH值,SOM,并且在典型的小叶章的软金属元素,诸如A1,铁,汞,铅,铜,和Mn的含量湿地,玉米田和三江平原稻田,采用的方法空间时间的替代品,探讨金属元素的含量和farmland.The结果表明开发湿地后,他们的个人资料分布特征改变了湿地被开发为耕地后,土壤中的有机质含量会被降低,随着pH的影响significantly.The SOM含量与仅铁相关,而pH为与soil.After大部分金属元素的湿地被回收作为水田正电或负相关,pH值在土壤上升,而A1,的Fe,和Pb被富集,并且Mn为丢失;它被开垦为旱地,pH值在土壤后降低,而A1,铁,和Pb被丢失,并且Mn为enriched.Hg在两者旱地和水田丢失,而在Cu中的变化是显着。湿地回收和培养导致pH条件的变化,这可能是导致土壤金属元素和它们的剖面分布的特征的内容的变化的主要因素。

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