六六六在土壤中持留和降解
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PERSISTENCE AND DEGRADATION OF BHC IN SOIL
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    摘要:

    本研究结果表明:(1)六六六在旱地土壤中的持留性一般比稻田土壤高;(2)土壤中六六六残留量的β/γ比值较大;(3)稻田土壤中六六六残留量很低。这主要是由于六六六在稻田土壤中的降解比旱地土壤快得多,以及β-666在土壤中比γ-666更稳定而造成的。实验表明不同作物对土壤中六六六残留量的吸收不同。稻米中六六六残留量与收割时土壤中残留量相关系数等于0.379,没有明显相关;而花生中残留量与土壤中残留量呈极显著相关。实验观察到六六六的降解速率随土壤水份、温度的增加而增加,适量的有机质能促进六六六在土壤中的降解作用。文章讨论了六六六在土壤中降解的可能历程。

    Abstract:

    Investigation showed that BHC residue in soil was characterized by higher persistence in upland soil than in paddy soil, greater ratio of β-isomer γ-isomer of BHC residue in soil and lower residue of BHC in paddy soil. These characteristics resulted from the higher rate of BHC degradation in paddy soil and higher stability of β-BHC in comparision with γ-BHC in soil. Expei-iznent results alsp showed that the amount of BHC residue absorbed by various crops was different. No significant correlation was found between the content of BHC in rice plant and its residue in soil during harvest. However, the content of BHC in peanut was significantly correlatal with BHC residue in soil during harvest (r=0.64,n=21). The degradation of SHC in soil was related to.soil moisture, temperature and organic matter. It was observed that the degradation rate of BHC was increased with the increase of moisture and temperature in soil;appropriate amoant of organic matter promoted degradation rate of BHC in soil.The possible pathway of degradatian of BHC in soil is discussed in this paper.

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张水铭,马杏法,安琼.六六六在土壤中持留和降解[J].土壤学报,1988,25(1):81-88. Zhang Shuiming, Ma Xingfa, An Qiong. PERSISTENCE AND DEGRADATION OF BHC IN SOIL[J]. Acta Pedologica Sinica,1988,25(1):81-88.

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  • 在线发布日期: 2013-02-25
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