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Degradation and Movement of Chlorate in Longan Plantations

机译:龙眼人工林中氯酸盐的降解和运动

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摘要

In 1998 it was found that chlorate was able to induce flowering in longan trees (Dimocarpus longan L.).Since then potassium chlorate have been used in most longan plantations all over Thailand.The maximum rate in the early years of application was approximately 500 g for a medium size tree. An environmental impact study on the effects of chlorate application was carried out in the year 2000. It was revealed that if farmers apply once a year chlorate is unlikely to accumulate over the years and the long-term effect on soil environment was nil. However,due to reasons which are being investigated the application rate has gradually been increased.In 2003 the maximum application dose for a medium size tree was approximately 2,000 g which is out of the scope of the above mentioned study. Consequently,there has been concern on the accumulation and leaching of residues through soil profiles and the risk of ground water contamination in the long run. Thus,a re-study on the environmental impact has been done. Movement and degradation of the heavily applied chlorate in four control plots on four representative soils were monitored over a period of two years. Samples of these four profiles at in various depths,ranging from 0 to 200 cm were taken and samples have been incubated with chlorate and chlorate degradation has been monitored under laboratory conditions. Additionally,residual chlorate on 42 commercial longan plantations was monitored. The results suggested that organic matter content was the most important factor influencing chlorate degradation. The degradation was observed to be very slow in soils with less than 0.2% of organic carbon,regardless of their textures. It was also found that chlorate moved relatively fast in well drained sandy soils. Therefore,a few months after application almost none of it was found at the depth above 80 cm but significant concentrations of the residues were found at a depth of 150-230 cm at two year period in sandy soils of the control plots. In loamy and clayey soils significant chlorate residues were found in a depth of less than 100 cm. Almost none of it was found deeper than 140 cm within the study period. Similar distributions of chlorate residues were found in soil profiles under the tree canopies in the commercial orchards with these kinds of soils.Consequently,methods to control the application rate have to be investigated. Furthermore,measures to eliminate chlorate residues after flowering of longan trees should be imposed in order to eliminate long term impacts and leaching of residues to the ground water in the long run. Application of any form of sugars was proven to be able to enhance the degradation of chlorate residues.
机译:1998年,发现氯酸盐能够诱导龙眼树(Dimocarpus longan L.)的开花,此后,泰国各地大多数龙眼种植园都使用氯酸钾,早期施用量最大为500 g用于中等大小的树。 2000年进行了关于氯酸盐施用效果的环境影响研究。结果表明,如果农民每年施用一次氯酸盐,多年以来就不太可能积累,对土壤环境的长期影响为零。但是,由于正在调查的原因,施用量逐渐增加。2003年,中型树的最大施用量约为2,000 g,超出了上述研究的范围。因此,从长远来看,人们一直关注残留物通过土壤剖面的积累和浸出以及地下水污染的风险。因此,已经对环境影响进行了重新研究。在两年的时间内,对四个代表性土壤上四个对照样地中大量施用的氯酸盐的移动和降解进行了监测。采集了从0到200 cm范围内不同深度的这四个剖面的样品,并将样品与氯酸盐一起孵育,并在实验室条件下监测了氯酸盐的降解。此外,监测了42个商业龙眼人工林中的残留氯酸盐。结果表明,有机物含量是影响氯酸盐降解的最重要因素。观察到在有机碳含量低于0.2%的土壤中,不管其质地如何,其降解过程都非常缓慢。还发现氯酸盐在排水良好的沙质土壤中移动相对较快。因此,施用后几个月,在对照样地的沙土中,在高于80 cm的深度几乎没有发现任何残留物,但是在两年的150-230 cm的深度发现了显着浓度的残留物。在壤土和黏土中,在小于100 cm的深度发现了大量的氯酸盐残留物。在研究期内几乎没有发现深度超过140厘米。在这类土壤的商业果园树冠下的土壤剖面中,氯酸盐残留物的分布也相似。因此,必须研究控制施用量的方法。此外,从长远来看,应采取措施消除龙眼树开花后的氯酸盐残留,以消除长期影响和残留物向地下水的淋溶。事实证明,使用任何形式的糖都可以促进氯酸盐残留物的降解。

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