黑钙土腐殖质状态指标与重金属迁移率的关系

V. Degtyarjov, O. Chekar
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引用次数: 1

摘要

腐殖质物质在重金属吸收和滞留中的特殊作用是一个重要的研究领域。目的是建立一些重金属流动形态的含量与土壤腐殖质指标参数之间的相关性,特别是研究活性腐殖质在调节土壤中重金属流动中的作用。研究指标:腐殖质总含量(以秋林为准);实际腐殖质物质的含量腐质(半分解,失去解剖结构的有机活性腐殖质(这部分腐殖质由于代谢吸收的钙在土壤中被钠取代而被peppep化)和被动腐殖质(完全去除钙后未被peppep化)的含量,被动腐殖质组成中实际腐殖质物质的含量(根据Sokolovsky)。研究重金属的流动形态(乙酸铵缓冲液pH 4,8萃取):锌;镉;镍;钴;铁;锰;铅;铜。研究地点:(1)在“Mykhailivska tsilyna”(苏梅地区)境内的典型黑钙质(钙- Voronic黑钙质sile1);土地用途选择:绝对处女地;被烧毁的处女地;林带;休耕的土地;耕地;(2)哈尔科夫地区-罗根站试验田黑钙质典型(钙质Voronic chernozem CL UE1);备选办法:休耕地、林带、可耕地;(a)未施肥;(b)矿物系统;(c)有机-矿物系统。通过相关分析,分别确定了0-10 cm和10-20 cm两个土层中重金属流动形态含量与腐殖质状态指标的相关性。在所有被调查的土地利用方案中,在“Mykhailivska tsilyna”的0-10厘米层中,锰、铜、锌、镉、铁的流动形式的含量与腐殖质的单独成分最密切相关。在罗根站0 ~ 10 cm土层中,腐殖质与铜、锌、钴、铅的流动形态含量关系最为密切。相反,在10-20 cm土层中则表现出其他特征。从先前除去活性腐殖质的土壤样品中提取的重金属明显多于从常规样品中提取的重金属。这是一种观点,认为活性腐殖质抑制重金属向土壤溶液的过渡,即降低重金属的流动性和植物的可及性。这种现象被称为活性腐殖质的“阻断功能”。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Relationship between humus condition indicators and mobility of heavy metals in chernozems
The special role of humus substances in the absorption and retention of heavy metals is an important area of research. The aim was to establish a correlation between the content of the mobile forms of some heavy metals and the parameters of soil humus indicators, in particular to investigate the role of active humus in regulating the mobility of heavy metals in the soil. The studied indicators: the total humus content (according to Tyurin); the content of the actual humus substances detritus (semi-decomposed, lost anatomical structure of organic the content of active humus (this the part of humus that can be peptized due to the replacement of metabolically absorbed calcium in the soil by sodium) and passive humus (that is not peptized after complete removal of calcium), the content of the actual humus substances in the composition of passive humus) (according to Sokolovsky). Investigated mobile forms of heavy metals (extraction with ammonium acetate buffer pH 4,8): zinc; cadmium; nickel; cobalt; iron; manganese; lead; cuprum. The research sites: (1) chernozem typical (Calcic Voronic Chernozem SiL UE1) on the territory of the «Mykhailivska tsilyna» (Sumy region); land use options: absolute virgin land; burnt-out virgin land; forest belt; fallow land; arable; (2) chernozem typical (Calcic Voronic Chernozem CL UE1) at the experimental field in Kharkiv region - Rogan station; options: fallow land, forest belt, arable land: (a) unfertilized; (b) the mineral system; (c) organo-mineral system. Correlation analysis was performed to identify the dependence of the content of mobile forms of heavy metals on the indicators of the humus state separately in two soil layers (0-10 and 10-20 cm). In the layer of 0-10 cm for «Mykhailivska tsilyna» in all investigated land use options the content of mobile forms of manganese, cuprum, zinc, cadmium, iron is most closely connected with separate components of humus, at the same time. In the soil of Rogan station in layer 0-10 cm the closest relationship can be traced between humus and the content of mobile forms of cuprum, zinc, cobalt and lead. On the contrary, in a layer of soil of 10-20 cm other features were shown. Significantly more heavy metals were extracted from soil samples from which active humus had been previously removed than from conventional samples. This is an argument that active humus inhibits the transition of heavy metals into the soil solution, ie, reduces the mobility of heavy metals and accessibility to plants. This phenomenon is called the "blocking function" of active humus.
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