摘要
利用不同类型土壤－水系统，加入一定量的ＫＮＯ＿３溶液，进行温度和冻融对脱氮化作用的影响以及亚硝酸盐积累规律的研究，培育实验结果表明，低温下，尤其是冻融条件下亚硝酸盐积累，是由于冻融加强有机质的分解及矿化作用所引起。将此结果用来解释克山病环境地球化学病因：急性克山病往往发生在冬春季节，这可能与冻融条件下水体中大量积累亚硝酸盐有关。
Effects of temperature and freezing-thawing on denitrifcation and accumulation of ni-trite in different soil-water systems were investigated.Incubation experimental results indi-cated that the accumulation of nitrite under low temperature,especially freezing-thawingconditions,is due to enhancing involvement of organic matter in mineralization by freezing-thawing events,which provided the available organic carbon compounds for denitrifyingbacteria,The results have been used to interpret Keshan disease environmental geochemicalpathonecy. Acute Keshan disease is usually prevalent in winter-spring seasons,related tothe accumulation of nitrite in large amounts in the water body under freezing-thawing condi-tions.
出处
《环境科学学报》
CAS
CSSCI
CSCD
北大核心
1995年第3期281-288,共8页
Acta Scientiae Circumstantiae
基金
国家自然科学基金
关键词
土壤
冻融
脱氮化作用
亚硝酸盐
积累
soil frezzing-thawing, denitrification, accumulation of nitrite.
