现代地质
現代地質
현대지질
GEOSCIENCE-JOURNAL OF GRADUATE SCHOOL CHINA UNIVERSITY OF GEOSCIENCES
2014年
3期
537-542
,共6页
秦爱华%于成广%李括%杨柯
秦愛華%于成廣%李括%楊柯
진애화%우성엄%리괄%양가
重金属%污染历史重建%柴河铅锌矿%辽宁
重金屬%汙染歷史重建%柴河鉛鋅礦%遼寧
중금속%오염역사중건%시하연자광%료녕
heavy metal%reconstruction of pollution record%Chaihe Pb-Zn deposit%Liaoning
通过对辽宁铁岭柴河铅锌矿及周边地区的土壤测量及柴河水库河漫滩沉积剖面的同位素测年研究,发现柴河铅锌矿开采导致的土壤重金属污染主要集中在柴河铅锌矿区周边3~5 km的范围内,土壤pH值表明土壤明显酸化。污染历史重建显示,1820年以来,随着沉积物中S含量的不断升高,其pH值累计下降2个单位;1900年以来河漫滩沉积物中的Cd、Pb、Zn累积明显;铅锌矿停止开采后,沉积剖面中Pb、Hg含量逐年降低;汇水域内的土壤酸化仍可导致土壤中累积的Cd和Zn对水库水体和库底沉积物造成二次污染,对水库鱼类的安全具有潜在风险。
通過對遼寧鐵嶺柴河鉛鋅礦及週邊地區的土壤測量及柴河水庫河漫灘沉積剖麵的同位素測年研究,髮現柴河鉛鋅礦開採導緻的土壤重金屬汙染主要集中在柴河鉛鋅礦區週邊3~5 km的範圍內,土壤pH值錶明土壤明顯痠化。汙染歷史重建顯示,1820年以來,隨著沉積物中S含量的不斷升高,其pH值纍計下降2箇單位;1900年以來河漫灘沉積物中的Cd、Pb、Zn纍積明顯;鉛鋅礦停止開採後,沉積剖麵中Pb、Hg含量逐年降低;彙水域內的土壤痠化仍可導緻土壤中纍積的Cd和Zn對水庫水體和庫底沉積物造成二次汙染,對水庫魚類的安全具有潛在風險。
통과대료녕철령시하연자광급주변지구적토양측량급시하수고하만탄침적부면적동위소측년연구,발현시하연자광개채도치적토양중금속오염주요집중재시하연자광구주변3~5 km적범위내,토양pH치표명토양명현산화。오염역사중건현시,1820년이래,수착침적물중S함량적불단승고,기pH치루계하강2개단위;1900년이래하만탄침적물중적Cd、Pb、Zn루적명현;연자광정지개채후,침적부면중Pb、Hg함량축년강저;회수역내적토양산화잉가도치토양중루적적Cd화Zn대수고수체화고저침적물조성이차오염,대수고어류적안전구유잠재풍험。
The heavy metal pollution of soil resulting from Pb-Zn mining mainly appears within 3 to 5 km around the mine area of Chaihe Pb-Zn deposit,Liaoning Province,and the pH value clearly reveals soil acidifi-cation of the region,thanks on the results from soil geochemical survey over the mining area of Chaihe Pb-Zn deposit and its surrounding area.History of heavy metal pollution reconstructed from the profile of overbank sedi-ment indicates that S concentration kept continueously increasing,and the pH dropped by 2 units since 1820 at the outlet of Chaihe reservoir.Whereas after 1900,Cd,Pb,and Zn in overbank sediment accumulated evident-ly,and the content of Pb and Hg in sediment profile declined after the cease of Pb-Zn mining.Soil acidification may remove Cd and Zn from accumulated in soil to water and sediment,and to result a potential risks to fish in Chaihe reservoir.