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为研究环丙酰草胺在土壤中的吸附迁移规律,分别采用批平衡法和柱淋溶法测定了环丙酰草胺在江西红壤、太湖水稻土、常熟乌杉土、陕西潮土和东北黑土5种土壤中的吸附和淋溶特性,并运用数学模型对其在土壤中的吸附及迁移特性进行了分析。结果表明:环丙酰草胺在5种土壤中的等温吸附曲线符合线性吸附方程,吸附常数Kd在1.41~7.08之间;环丙酰草胺在5种土壤中的淋溶性大小依次为:东北黑土>陕西潮土>常熟乌杉土>太湖水稻土>江西红壤。通过对吸附常数Kd与土壤有机质含量和pH值的关系进行分析,发现土壤pH值在吸附过程中属主要因素,Kd与土壤pH值呈负相关。上述结果表明,环丙酰草胺在供试的5种土壤中比较容易迁移,影响其迁移的主要因素是土壤pH值。环丙酰草胺在使用过程中应关注其对地表水和地下水造成的风险。 相似文献
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为评价环酰菌胺在土壤中的生态风险,采用超高效液相色谱-串联质谱(UPLC-MS/MS)方法测定了土壤和水中环酰菌胺的残留量,研究了该农药在红壤和水稻土中的吸附及降解特性,并对其淋溶特性进行了分析,评估了该农药对地下水的污染风险。结果表明:环酰菌胺在红壤和水稻土中的吸附符合Freundlich吸附等温线方程,KOC值分别为373.69和726.86 mL/g,水稻土对环酰菌胺的吸附能力强于红壤。好氧条件下,环酰菌胺在红壤和水稻土中的降解半衰期分别为0.63和5.06 d,积水厌氧条件下的降解半衰期分别为6.80和9.24 d,表明环酰菌胺在好氧条件下降解较快。环酰菌胺在红壤和水稻土中的地下水污染指数(groundwater ubiquity score)分别为1.19和1.10,表明其对地下水的污染风险较低。结果可为环酰菌胺的生态风险评估提供参考。 相似文献
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农药在土壤中的吸附和淋溶特性是评价其环境行为的重要指标。采用批量平衡法和土柱淋溶法,研究了双氟磺草胺在小麦种植区3种代表性土壤中的吸附和淋溶特性。结果表明:双氟磺草胺在安徽黏土、山东砂质壤土和河南砂质黏壤土中的吸附规律均可以较好地用Freundlich方程描述,其吸附系数(Kf)在0.39~0.62之间;土壤有机碳归一化吸附系数(Koc)在66.91~81.35之间,表明双氟磺草胺在3种土壤中均属于难吸附型;吸附自由能(ΔG)在-10.90~-10.42kJ/mol之间,均属于物理吸附。双氟磺草胺在3种土壤中的淋出率在71.7%~74.1%之间,说明其在3种土壤中的淋溶性均较强。双氟磺草胺初始添加量和腐殖酸对淋出率具有一定影响。综合试验结果,认为双氟磺草胺在3种土壤中的吸附和淋溶可能受土壤有机质含量、黏粒含量、阳离子交换量和土壤pH值等多个因素的综合影响,其对地下水的污染风险较大,因此应引起高度重视。 相似文献
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实验室条件下,初步研究了手性农药三唑醇及其非对映异构体三唑醇A(对映异构体1R,2S体和1S,2R体的混合物)与三唑醇B(对映异构体1R,2R体和1S,2S体的混合物)在浙江杭州潮土(有机质含量1.90%,pH 6.85)、金华水稻土(有机质含量1.63%,pH 4.94)和兰溪红土(有机质含量0.38%,pH 4.03)中的降解动态及对映体之间相互转化的情况。结果表明:三唑醇在潮土、水稻土和红土中的降解半衰期分别为56.4、105.0和154.0 d,180 d时降解率分别为91.9%、79.2%和57.7%;三唑醇在潮土中发生两次三唑醇A体向B体转化和1次三唑醇B体向A体的转化,而在水稻土和红土中,三唑醇A体与B体之间相互各转化1次。表明三唑醇对映异构体的降解动态因土壤性质不同而存在差异。研究结果为三唑醇的科学合理使用及其环境风险评估提供参考。 相似文献
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为合理评估除草剂异唑草酮的环境风险,在实验室模拟条件下,研究了异唑草酮在土壤 (红壤土)表面光解以及在不同质地土壤 (潮土、水稻土和红壤土) 中的降解和淋溶特性。结果表明:异唑草酮在土壤表面的光解遵循一级反应动力学方程ct = 4.23e–0.008t (r = 0.937),半衰期为82.5 h;其在潮土、水稻土和红壤土中的降解均符合一级动力学方程,好氧条件下,异唑草酮在3种土壤中的降解半衰期分别为10.5、43.3和139 h,厌氧条件下的降解半衰期分别为19.4、18.4和158 h;其在潮土、水稻土和红壤土中的淋溶系数 (Rf) 分别为0.417 0、0.083 3和0.083 3。研究表明:异唑草酮在土壤表面光解速率较慢,而在土壤中好氧及厌氧条件下降解速率均较快,残留期短;其在土壤中淋溶性较弱,不易对周围环境及地下水造成污染风险。 相似文献
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吸附是农药在土壤环境中行为和归宿的重要过程,农药在土壤矿物上的吸附直接影响其在土壤中的迁移、转化和生物利用等过程。了解农药在土壤中的吸附,对于预测和评价农药对土壤、地下水存在的潜在危害,开展土壤修复具有十分重要的意义。本研究通过批量平衡试验,研究了苯噻酰草胺在海泡石和凹凸棒石中的吸附行为及机理。结果表明:苯噻酰草胺在海泡石和凹凸棒石中的吸附分为快速反应阶段和慢速平衡阶段,吸附平衡时间约为6 h。其吸附动力学曲线符合准二级动力学方程,线性方程和Freundlich吸附等温方程能较好地描述其在海泡石和凹凸棒石中的吸附行为,海泡石对苯噻酰草胺的吸附容量高于凹凸棒石。傅立叶变换红外光谱(FTIR)和X-射线衍射(XRD)分析显示:苯噻酰草胺在海泡石和凹凸棒石中的吸附不仅发生在其表面层,还进入了其内层。机理分析推测:苯噻酰草胺主要是通过氢键、电荷转移和电荷-偶极键形式吸附在黏土矿物中。 相似文献
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中国政府已同意给予先正达的除草剂甲基磺草酮(mesotrione)和巴斯夫的啶酰菌胺(boscalid)行政保护。保护期7.5年。国家发展与改革委员会最近批准7.5年的保护期不再延长。 相似文献
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Biodegradation of [ring-14C] mecoprop (2-(4-chloro-2-methylphenoxy)propionic acid) was determined in surface and sub-surface soil at concentrations of 0·0005, 0·05, 0·5, 5, 50, 500, 5000 and 25000 mg kg-1. The kinetics of mineralisation were evaluated from the mineralisation rates as a function of time and by non-linear regression analysis. In the sub-surface soil, degradation was 6–8 times slower than in surface soil, but the shape of the curves was the same in both layers. At concentrations between 0·0005 and 0·5 mg kg-1, in both surface and sub-surface soil, degradation was initially zero-order followed by first-order kinetics. At 5 to 500 mg kg-1 in surface soil and 5 to 50 mg kg-1 in sub-surface soil the degradation rate was initially either constant or decreasing followed by exponential degradation indicating increasing populations of mecoprop decomposers in the soil. At 5000 and 25000 mg kg-1 in the surface soil and at 500, 5000 and 25000 mg kg-1 in the sub-surface soil, the degradation was negligible, as determined by the percentage [14C] carbon dioxide evolved. By non-linear regression, the three-half order model was found to describe the mineralisation. © 1998 SCI 相似文献
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Subhasish K Chakraborty Anjan Bhattacharya Ashim Chowdhury 《Pest management science》1999,55(9):943-948
Residual fate and behaviour of the herbicide oxadiazon in Kalyani soil, paddy straw and grain were studied under subtropical conditions, in West Bengal following application @ 1 kg and 2 kg ha−1. Dissipation of oxadiazon in soil followed first-order kinetics and DT50 values ranged from 44 to 45 days. Residues at harvest in paddy grains and straw were also studied. Degradation of oxadiazon after 60 days of incubation at 28(± 1) °C in alluvial soil at water holding capacity yielded 10 metabolites of which four were characterised by spectroscopy. © 1999 Society of Chemical Industry 相似文献
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磺酰脲类除草剂的降解机制及代谢产物的研究进展 总被引:6,自引:0,他引:6
磺酰脲类除草剂是一类高效,低毒和高选择性的除草剂,该类除草剂能有效防除阔叶杂草,其中有些品种对禾本科杂草也有一定的抑制作用。但同时因其用量低、对哺乳动物低毒以及独特的除草活性等特点而得到广泛应用。因此,了解磺酰脲类除草剂在土壤中的环境行为及归趋对于其科学合理使用、防止作物药害和保护农业生态环境具有非常重要的意义。根据笔者对磺酰脲类除草剂的深入研究,并总结归纳国内外的相关文献报道,对磺酰脲类除草剂的降解机制及其代谢产物的研究进行了综述,最后展望了磺酰脲类除草剂未来的发展趋势。 相似文献
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Atrazine behaviour was investigated in the different pedological horizons from profiles of two non-tilled soils, a Typic Argiustoll and an Entic Haplustoll from the Argentinean pampas. As atrazine use in field conditions was associated with maize cropping, only one type of soil received atrazine every other year. Atrazine behaviour was characterized through the balance of 14C-U-ring atrazine radioactivity among the mineralized fraction, the extractable fraction and the non-extractable bound residues. The composition of the extractable fraction was characterized. Atrazine mineralization was the main dissipation mechanism in the superficial horizon of the Argiustoll because of microbial adaptation after repeated atrazine applications. In contrast, little atrazine mineralization was found in the Haplustoll profile, and it decreased with depth. The capacity of the soil organic matter to form bound residues was characterized using soil-size fractionation. Atrazine-bound residues depended on the soil organic matter content and the size of the fraction. Organic matter in the largest size fractions had a higher capacity to form atrazine-bound residues. In the Argiustoll profile, the atrazine degradation capacity decreased in the subsurface horizons (Bt1 and Bt2), where a large part of bound residues were formed. The deepest horizon (BC) of this profile had a high capacity to degrade atrazine reaching this horizon after a lag period. In the Haplustoll profile, atrazine mineralization and bound residue formation followed the organic carbon mineralization pattern. 相似文献
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高寒草甸不同类型草地土壤机械组成及肥力比较 总被引:3,自引:0,他引:3
研究了青藏高原高寒草甸不同类型草地土壤机械组成和土壤养分变化特征,并用相关分析探讨了土壤理化特征、土壤机械组成对不同草地类型群落物种组成、生物量变化的响应。结果表明:不同草地类型土壤机械组成分布大致是矮嵩草草甸:粉粒>细砂粒>粘粒>粗砂粒;高山嵩草草甸:细砂粒>粉粒>粘粒>粗砂粒;藏嵩草沼泽化草甸:细砂粒>粉粒>粘粒>粗砂粒;金露梅灌丛:粉粒>粘粒≥细砂粒>粗砂粒。矮嵩草草甸、高山嵩草草甸为粉砂质粘壤土,藏嵩草沼泽化草甸为壤土,金露梅灌丛为壤质粘土。矮嵩草草甸、高山嵩草草甸和金露梅灌丛土壤颗粒分布相对比较均匀(除藏嵩草沼泽化草甸外),主要集中在<0.5mm的范围内,土壤粘粒含量普遍大于20%。土壤全量养分和速效养分以及土壤物理特征均影响着高寒草甸不同草地类型土壤质量和土壤结构。土壤结构和养分状况是判断高寒草甸生态系统生态功能维持的关键指标之一。 相似文献