摘要
土壤对Hg ̄(2+)有自净力,其作用实质是Hg的形态转化.本研究试验了膨润土、腐殖质、碳酸钙对汞形态转化的影响.结果表明,膨润土是使Hg ̄(2+)迅速向残留态转化而降低作物对汞的吸收,其效果在用量为0─450g/kg范围呈线性增长;腐殖质使Hg ̄(2+)迅速向腐殖质态汞转化,且有与矿质粘粒争夺Hg ̄(2+)之势,故最适用量因土壤粘粒含量而异;碳酸钙也使Hg ̄(2+)向残留态转化,对酸性土的最佳用量,以使土壤的钙饱和度达到50%—85%为好。
The influences of bentonite,humus and CaCO_3 on transformation of mercury in soilwere investigated. The results showed that bentonite, humus, and CaCO_3 are able to stimu-late the transformation of Hg from ion to other bonding forms and consequently depress ad-sorption of Hg by plant. Bentonite depressed the Hg adsorption linearly correlated with itscontent within a range of 0─450 g/kg.Humus competed with soil clay for Hg ̄(2+) and the re-lation of content-response correlated with clay content of the sample. CaCO_3 was effective todepress plant Hg uptake from soil under certain conditions.The mechanism of CaCO_3 issomewhat similar to that of bentonite.
出处
《环境科学学报》
CAS
CSSCI
CSCD
北大核心
1995年第2期148-155,共8页
Acta Scientiae Circumstantiae
基金
国家教委基金
关键词
土壤
汞
形态
活性抑制
陆生食物链
soil
Hg activity depress
terrestrial food chain.