Lsmail B S, Choo Lee Yin, Salmijah S, Halimah M, Tayeb M A
J Environ Biol. 2015 Sep;36(5):1105-11.
The sorption and desorption of cyfluthrin mixture isomers were determined using batch equilibration method and mobility was studied under laboratory conditions, using packed soil column. The soil types used in the study were clayey, clay loam and sandy clay loam obtained from three tomato farms in Cameron Highlands. A low Freundlich adsorption distribution coefficient K(ads(f)) for cyfluthrin was observed for clayey, clay loam and sandy clay loam soils (95.69, 21.64 and 8.99 l/kg, respectively). Results showed that cyfluthrin had high Freundlich organic matter (OM) distribution coefficient K(oc) values of 5799, 2278 and 1635 lkg(-1) for clayey, clay loam and sandy clay loam soils, respectively. These values indicate that cyfluthrin is considered immobile in Malaysian soils with different textures, based on the value of K(oc) by McCall. Adsorption of cyfluthrin was significantly (P < 0.05) affected with soil pH, fertilizer NPK, organic matter content and temperature. It was observed that approximately 95.8%, 93.8% and 91.8% of the adsorbed cyfluthrin remained sorbed after four successive rinses for clayey, clay loam and sandy clay loam soils. Soil column test showed that cyfluthrin was not detected in leachate. Cyfluthrin was detected in topsoil and its concentration decreased with depth. The downward movement of cyfluthrin in sandy clay loam soil was more than that in clay loam and clayey soils. Approximately, 80.9%, 77.8% and 67.3% cyfluthrin was observed at the depth of 0-5 cm (rainfall 350 mm) for clayey, clay loam and sandy clay loam soils respectively. Mobility of cyfluthrin showed that the percentage of cyfluthrin leached into soil was not affected by the amount of rainfall. The result clearly showed that cyfluthrin molecules were bound strongly to all the three Malaysian soil types.
采用批量平衡法测定了氟氯氰菊酯混合物异构体的吸附和解吸情况,并在实验室条件下使用填充土柱研究了其迁移性。研究中使用的土壤类型为从金马仑高原三个番茄农场获取的黏土、黏壤土和砂质黏壤土。对于黏土、黏壤土和砂质黏壤土,观察到氟氯氰菊酯的弗罗因德利希吸附分配系数K(ads(f))较低(分别为95.69、21.64和8.99 l/kg)。结果表明,对于黏土、黏壤土和砂质黏壤土,氟氯氰菊酯的弗罗因德利希有机质(OM)分配系数K(oc)值分别较高,为5799、2278和1635 lkg(-1)。根据麦考尔的K(oc)值,这些数值表明氟氯氰菊酯在马来西亚不同质地的土壤中被认为是不易迁移的。氟氯氰菊酯的吸附受到土壤pH值、肥料NPK、有机质含量和温度的显著影响(P < 0.05)。观察到,对于黏土、黏壤土和砂质黏壤土,在连续四次冲洗后,大约95.8%、93.8%和91.8%被吸附的氟氯氰菊酯仍被吸附。土柱试验表明,渗滤液中未检测到氟氯氰菊酯。在表土中检测到氟氯氰菊酯,其浓度随深度降低。氟氯氰菊酯在砂质黏壤土中的向下迁移比在黏壤土和黏土中更多。对于黏土、黏壤土和砂质黏壤土,在0 - 5 cm深度(降雨量350 mm)处分别观察到约80.9%、77.8%和67.3%的氟氯氰菊酯。氟氯氰菊酯的迁移性表明,淋溶到土壤中的氟氯氰菊酯百分比不受降雨量的影响。结果清楚地表明,氟氯氰菊酯分子与所有三种马来西亚土壤类型紧密结合。