地质通报
地質通報
지질통보
GEOLOGICAL BULLETIN OF CHINA
2014年
8期
1188-1195
,共8页
张江华%王葵颖%李皓%陈华清%柯海玲%刘瑞平%赵阿宁
張江華%王葵穎%李皓%陳華清%柯海玲%劉瑞平%趙阿寧
장강화%왕규영%리호%진화청%가해령%류서평%조아저
生物有效性%土壤%Pb%Cd%金矿区
生物有效性%土壤%Pb%Cd%金礦區
생물유효성%토양%Pb%Cd%금광구
bioavailability%soil%Pb%Cd%gold ore district
土壤中重金属形态与其赋存条件之间的关系是评估土壤重金属风险的关键问题。以受金矿开发影响的土壤中Pb、Cd为研究对象,采用动力学方程分析了土壤有机质、粘粒、pH、Eh等对Pb、Cd生物有效性的影响。结果表明,研究区影响Pb、Cd生物有效性的主要因素有土壤有机质、pH及Eh;有机质与土壤中的Pb、Cd总量呈现正相关性;但当有机质含量增加时,Pb、Cd的水溶态和离子交换态含量反而降低;土壤粘粒对Pb、Cd生物有效性的影响不甚明显;虽然较低的土壤pH值会加剧重金属离子的活性,增强其生物有效性,但过高的pH值又会提高Cd碳酸盐态、铁锰氧化态的含量;Pb、Cd生物有效性随着土壤氧化-还原电位的降低而减弱。研究发现,对于Pb、Cd污染的土壤,通过增施有机肥可提高农产品的安全性;保持土壤处于弱酸-弱碱有利于降低农产品风险;在农作物成熟期实施淹水灌溉,降低土壤氧化-还原电位,可抑制Pb、Cd在籽粒中的累积。
土壤中重金屬形態與其賦存條件之間的關繫是評估土壤重金屬風險的關鍵問題。以受金礦開髮影響的土壤中Pb、Cd為研究對象,採用動力學方程分析瞭土壤有機質、粘粒、pH、Eh等對Pb、Cd生物有效性的影響。結果錶明,研究區影響Pb、Cd生物有效性的主要因素有土壤有機質、pH及Eh;有機質與土壤中的Pb、Cd總量呈現正相關性;但噹有機質含量增加時,Pb、Cd的水溶態和離子交換態含量反而降低;土壤粘粒對Pb、Cd生物有效性的影響不甚明顯;雖然較低的土壤pH值會加劇重金屬離子的活性,增彊其生物有效性,但過高的pH值又會提高Cd碳痠鹽態、鐵錳氧化態的含量;Pb、Cd生物有效性隨著土壤氧化-還原電位的降低而減弱。研究髮現,對于Pb、Cd汙染的土壤,通過增施有機肥可提高農產品的安全性;保持土壤處于弱痠-弱堿有利于降低農產品風險;在農作物成熟期實施淹水灌溉,降低土壤氧化-還原電位,可抑製Pb、Cd在籽粒中的纍積。
토양중중금속형태여기부존조건지간적관계시평고토양중금속풍험적관건문제。이수금광개발영향적토양중Pb、Cd위연구대상,채용동역학방정분석료토양유궤질、점립、pH、Eh등대Pb、Cd생물유효성적영향。결과표명,연구구영향Pb、Cd생물유효성적주요인소유토양유궤질、pH급Eh;유궤질여토양중적Pb、Cd총량정현정상관성;단당유궤질함량증가시,Pb、Cd적수용태화리자교환태함량반이강저;토양점립대Pb、Cd생물유효성적영향불심명현;수연교저적토양pH치회가극중금속리자적활성,증강기생물유효성,단과고적pH치우회제고Cd탄산염태、철맹양화태적함량;Pb、Cd생물유효성수착토양양화-환원전위적강저이감약。연구발현,대우Pb、Cd오염적토양,통과증시유궤비가제고농산품적안전성;보지토양처우약산-약감유리우강저농산품풍험;재농작물성숙기실시엄수관개,강저토양양화-환원전위,가억제Pb、Cd재자립중적루적。
The relationship between morphology and occurrence conditions of heavy metals is key to assessing the risk of heavy metals in soil. In this paper, the authors studied Pb and Cd soil related to gold mining, analyzed the impact of such factors as organic matter, clay, pH and Eh in soil on bioavailability by means of the kinetic equation. The results show that the main factors affecting bioavailabil-ity are soil organic matter, pH and Eh. The content of organic matter has a distinct relationship with Pb or Cd in soil.Also, the in-crease in clay content in soil may slightly increase the proportion of the content of Cd and Pb in the ionic exchangeable form to the total content of Pb and Cd. The soil acidification may increase the content of cadmium in the ionic exchangeable form, which has a distinct relationship with the pH in soil. Bioavailability is weakened with decreasing soil Eh. It is obvious that the increase in organic matter in soil may obviously reduce the content of Cd and Pb in the ionic and exchangeable form. When the effective state is consid- ered, the maintenance of soil weak acidification or weak alkalinity is a good way to avoid active bioavailability. When the crops ma-ture, the implementation of flood irrigation can inhibit the accumulation of heavy metals in grain.