有机物料对土壤中水溶性氟环境效应的影响  

The environmental effect of organic materials on soil soluble fluorine

作　　者：王开勇[1] 杨乐[1] 赵天一[2] 黎成厚[2] 张凤华[1] 杨斌[2] 降巧龙[2] 

机构地区：[1]石河子大学农学院,新疆石河子832003 [2]贵州大学生命科学学院,贵州贵阳550025

出　　处：《生态环境》2007年第3期879-882,共4页Ecology and Environmnet

基　　金：国家重点基础研究发展计划项目(2006CB708401);石河子大学自然科学基金项目(ZRKX2006-Q22)

摘　　要：土壤是固、液、气三相共存体,氟在土-水-植物、动物界面的转化可通过土壤水溶性氟含量表征。试验选用典型贵州黄壤和石灰土,运用有机质进行土壤污染修复的机理,通过向模拟高氟污染土壤中添加有机物料泥炭和风化煤,采用两因素最优设计,研究两种有机物料对土壤中水溶性氟含量的影响。结果表明,泥炭和风化煤都能降低土壤中水溶性氟含量,且泥炭的处理效果更好,最佳添加量是1.258g·kg-1。同时表明,黄壤和石灰土环境下氟形态转化的化学机理不同,运用有机质修复氟污染黄壤添加适量就可达到理想效果,而氟污染石灰土还存在其它更直接有效的方法改变氟在石灰土环境下的形态及其活性。Fluorine transformation in soil-water-plant and animal system can be represented by soil soluble fluorine content. This research was based on mechanism that organic material has reconditions action on soil pollution. We chose yellow soil and calcareous soil in Guizhou province, peat coal and gentle breeze coal were added into simulated high fluorine polluted soil to study the effect of organic material on soil soluble fluorine content using the qualified design. The results indicate that both peat coal and gentle breeze coal can decrease soluble fluorine content in soil, while the reconditions action of peat coal was better than gentle breeze coal and the optimum added level of peat coal was 1.258 g·kg^-1. It was found that chemistry mechanism of fluorine conformation transformation were different in yellow soil and calcareous soil circumstance. By applying suffice quantum of organic material can be reconditioned and achieve ideal effect in fluorine polluted yellow soil. Whereas by changing configuration and activity of fluorine was necessary in fluorine polluted calcareous soil circumstance.

关 键 词：土壤水溶性氟 泥炭 风化煤 有机质 

分 类 号：X53[环境科学与工程—环境工程]