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Effect of microbial activity, soil water content and added copper on the temporal distribution patterns of HCB and DDT among different soil organic matter fractions

机译:微生物活性,土壤含水量和添加铜对不同土壤有机质组分中六氯苯和滴滴涕时间分布格局的影响

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Temporal changes in the distribution of exogenous HCB and DDT among different soil organic matter fractions were studied under sterile and non-sterile conditions, different soil water contents, and different concentrations of added Cu~(2+). The residence time was 311 days. Soil organic matter was fractionated into fulvic acid (FA), humic acid (HA), bound-humic acid (BHA), lipid, and insoluble residue (IR) fractions by a methyl isobutyl ketone (MIBK) method. Results revealed that there is a mass transfer tendency of DDT and HCB from FA, HA and BHA to IR and lipid fractions with increasing residence time. Microbial activity accelerated the mass transfer, while the addition of Qr~+ slowed it down. The HCB and DDT transfer rate decreased as the soil moisture increased from 1.9% to 60%, but increased when soil moisture increased further to 90%. A two-compartment first order kinetic model was used to describe the mass transfer from FA, HA and BHA.
机译:研究了在无菌和非无菌条件下,不同土壤含水量和不同Cu〜(2+)添加浓度下,不同土壤有机质组分中外源HCB和DDT分布的时空变化。停留时间为311天。通过甲基异丁基酮(MIBK)方法将土壤有机物分为富里酸(FA),腐殖酸(HA),结合腐殖酸(BHA),脂质和不溶性残留物(IR)馏分。结果表明,随着停留时间的增加,DDT和HCB从FA,HA和BHA到IR和脂质组分的质量转移趋势。微生物活性加速了传质,而Qr〜+的加入则减慢了传质。 HCB和DDT的转移速率随着土壤水分从1.9%增加到60%而降低,但是当土壤水分进一步增加到90%时增加。使用两室一阶动力学模型描述了FA,HA和BHA的传质。

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