噻虫嗪在农田土壤中环境行为的研究进展

噻虫嗪是当前全球销售量最大的新烟碱类农药之一，随着噻虫嗪的广泛使用，噻虫嗪在土壤环境中的迁移转化和归宿问题成为研究热点。本文总结了噻虫嗪对陆生生物（蜜蜂、蚕、蚯蚓、鹌鹑）、水生生物（藻类、大型溞、斑马鱼等）以及土壤微生物的影响，系统综述了噻虫嗪在农田土壤中的残留、降解、吸附解析以及迁移与淋溶等环境行为及主要影响因素，并指出了噻虫嗪在农田土壤中环境行为相关研究存在的不足以及未来研究应该关注的重点和方向，以期为噻虫嗪的科学安全使用以及保障农田土壤生态环境健康提供科学依据。     

间歇灌溉对稻田毒死蜱迁移转化特征的影响

间歇灌溉作为丘陵区稻田常见的灌溉方式之一,其强烈的干湿交替过程会影响稻田中污染物的环境行为。在室内批量平衡吸附试验的基础上,通过农药野外喷施试验与动态观测,研究了间歇淹水和持续淹水条件下石灰性紫色土发育的稻田中毒死蜱的迁移转化特征。结果表明,土壤对毒死蜱的吸附能力远远强于其对毒死蜱主要降解产物3,5,6-三氯-2-吡啶醇(3,5,6-TCP)的吸附能力,毒死蜱的吸附容量常数范围为34~170,TCP的吸附容量常数范围为0.62~0.67,且对毒死蜱和TCP的吸附容量常数及分配系数均以耕作层土壤高于非耕作层土壤;施药后田面水中毒死蜱及TCP的浓度均随时间迅速下降,两者均可通过土壤大孔隙优先流快速迁移至50cm深处;间歇灌溉处理稻田土壤孔隙水中两者的浓度总体低于持续淹水处理;降雨和灌溉事件会导致两者由土壤固相迅速向水相发生短时间、高浓度释放与淋失。     

CMC粘接法制备柱状成型活性炭

以羧甲基纤维素钠(CMC)为粘接剂制备了柱状成型活性炭,研究了炭化温度、CMC添加量对产物吸附性能、孔结构及强度的影响。结果表明,随着炭化温度的升高,柱状成型活性炭的比表面积、亚甲基蓝吸附值和碘吸附值均呈现下降趋势;随着CMC添加量的增加,柱状成型活性炭的比表面积、总孔容、微孔容、平均孔径及亚甲基蓝吸附值、碘吸附值及对甲苯的吸附能力均逐渐降低,其强度逐渐增大。CMC粘接法制备柱状成型活性炭的最佳工艺为炭化温度200℃,CMC添加量10%,产物比表面积可达844.9 m2/g,亚甲基蓝吸附值和碘吸附值分别为189.2及968.2 mg/g,强度可达99.83%,甲苯的吸附率达65.5%。     

The Magnesium Status of Some Fiji Soils

Abstract

Magnesium (Mg) is an essential macronutrient element for all living organisms, but literature reports of Mg deficiency in agriculture and forestry appear regularly. In many tropical areas, Mg is added to soils by using dolomitic limestone and as minor additions through impurities in some fertilizers. Minimal information is available on the Mg status of Fiji soils, and deficiencies have been observed in some crops. This study investigated the Mg status of a range of Fiji soils and found that major agricultural soils of Fiji contain variable amounts of Mg, both in the total concentrations and in the different forms of the element present. The variations can be related to the soil parent materials, degree of weathering, clay content, and mineralogy. Low plant‐available Mg concentrations are present in many of the highly weathered soils with limited reserves present. Development of intensive agriculture should consider Mg when developing fertilizer programs.     

套种不同牧草的果园土壤对铵的吸附特性研究

以套种不同牧草的果园土壤为研究对象,通过室内等温吸附实验,分析比较了各个处理对氨态氮的吸附特性,并将结果用不同的数学模型拟合进行分析.结果表明:当土壤的氨浓度超过一临界值时,其对氨离子的吸附量会出现明显上升,而在此临界值以下则变化不明显；套种不同牧草可不同程度地提高土壤的铵吸附能力,具体表现为圆叶决明＞百喜草＞平托花生＞宽叶雀稗＞CK(自然生日本草)；各处理土壤铵等温吸附与多项式拟合效果最佳,与Freundlich、Temkin方程拟合达显著水平,Langmuir方程的拟合结果较差.     

活性炭对柴油机尾气吸附机理及其行为研究

柴油车排放尾气严重污染环境并危害人类健康，其净化技术一直是人们研究的热点问题。基于各种活性炭的尘埃吸附性及气体通透性．研究了不同量活性炭在非催化条件下对尾气的吸附机理及行为。试验结果表明：各种活性炭对柴油机尾气排放物吸附作用较为明显：煤质活性炭对于尾气排放物吸附作用要强于椰壳活性炭碳，且对尾气排放降低程度最大、经济性最好用量在400g左右。     

花生壳残渣制备活性炭及吸附性能测定

用提取黄酮后废弃的花生壳做原料,选择不同的活化剂在一定温度下制备活性炭,并且测定其吸附性能。结果表明：磷酸作为活化剂时活性炭产率最高,达39.5%;当炭化温度为500℃、活化剂为氢氧化钾或磷酸、活化剂浓度为10%时,碘吸附值最高,为966.7mg/g;当炭化温度为500℃、活化剂浓度为10%时,几种活化剂制备出来的活性炭亚甲基蓝脱色力均达到40mL/g左右;与几种市售活性炭比较,花生壳活性炭碘吸附值能够满足市场需要,但是亚甲基蓝脱色力偏低;相同条件下,盐作为活化剂所制备出的活性炭对镍离子的吸附能力比较稳定。     

Long-Term Effect of Fertilizer and Rice Straw on Mineral Composition and Potassium Adsorption in a Reddish Paddy Soil

Increasing K⁺ adsorption can be an effective alternative in building an available K pool in soils to optimize crop recovery and minimize losses into the environment. We hypothesized that long-term fertilization might change K⁺ adsorption because of changes in the chemical and mineralogical properties of a rice (Oryza sativa L.). The aims of this study were (i) to determine clay minerals in paddy soil clay size fractions using X-ray diffraction methods and a numerical diagram-decomposition method; (ii) to measure K⁺ adsorption isotherms before and after H₂O₂ oxidation of organic matter, and (iii) to investigate whether K⁺ adsorption is correlated with changes in soil chemical and mineral properties. The 30-yr long-term fertilization treatments caused little change in soil organic C (SOC) but a large variation in soil mineral composition. The whole-clay fraction (<5 μm) corresponded more to the fertilization treatment than the fine-clay fraction (<1 μm) in terms of percentage of illite peak area. The total percentage of vermiculite-chlorite peak area was significantly negatively correlated with the total percentage of illite peak area in the <5 μm soil particles (R=-0.946, P<0.0006). Different fertilization treatments gave significantly different results in K⁺ adsorption. The SOC oxidation test showed positive effects of SOC on K⁺ adsorption at lower K⁺ concentration (?120 mg L^?1) and negative effects at higher K⁺ concentration (240 mg L^?1). The K⁺ adsorption by soil clay minerals after SOC oxidization accounted for 60–158% of that by unoxidized soils, suggesting a more important role of soil minerals than SOC on K⁺ adsorption. The K⁺ adsorption potential was significantly correlated to the amount of poorly crystallized illite present (R=0.879, P=0.012). The availability of adsorbed K⁺ for plant growth needs further study.     

pH值对重金属Pb~(2+)吸附特性的影响

以砂壤土为研究对象,采用1次平衡法,研究了pH值对重金属Pb2+吸附特性的影响,在此基础上对等温吸附进行模拟分析。结果表明,土壤对Pb2+吸附的pH值影响敏感阈值范围为pH7。所引入的平衡质量体积比与吸附量之间的模型ln(S)=K1×CK2能较好地模拟不同pH值条件下的等温吸附规律。其次为Freundilich模型,Henry模型较适用于低pH值条件下的模拟分析。     

Retention of Molybdenum(VI) by Three Finnish Mineral Soils

Abstract

Retention of molybdate by three Finnish mineral soils from 10^?4 and 10^?5 M sodium molybdate solutions at room temperature was investigated at pH 2.3–7.5. In the adsorption experiments 0.02 M KCl was used as ionic medium, and the samples were left to equilibrate for 72 h. The solid: solution ratio was 1:100 (w: v). Maximum adsorption occurred below pH 4.5, where about 60–80 % of added molybdenum was retained. Desorption of the adsorbed molybdenum was measured by adding 50 ml of 0.02 M KCl into weighed soil samples and shaking for 17 h in an apparatus with a mechanical stirrer. In each soil an appreciable amount of Mo was so tightly bound that it could not be removed by KCl treatment.