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ASSESSMENT OF POTENTIAL NUTRIENT RELEASE FROM DREDGING ACTIVITIES

机译:疏D活动对潜在营养释放的评估

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摘要

Concerns about management of dredged material and its environmental effect on water quality are constantly increasing in Thailand. One of the major concerns is the release of nutrients from dredged spoils and the consequent effects of eutrophication. There are two major modes of potential nutrient release from dredging activities. The first results from release of pore water nutrients when dredge spoil is deposited in the bay as a disposal option and the other is the direct flux of nutrients from deep sediments that are exposed when dredge material is removed. The nutrient release was determined by collecting sediment cores from the mouth of the Tachin River (Thailand) and analyzing for nutrient concentrations in pore water to estimate the maximum nutrient release during disposal. A flux experiment was also conducted with deep sediment core sections (simulating exposed sediment) to examine changes in nutrient release over a 24-hour period. The results show an extremely high initial flux of ammonium, which decreased rapidly to ambient surface sediment flux rates. Despite high phosphate concentrations in the pore water, the high rate of sediment oxidation of iron sul-fide minerals resulted in a minimal release of phosphate.
机译:在泰国,对挖出物的管理及其对水质的环境影响的关注在不断增加。主要关注点之一是疏dr的土壤中养分的释放以及富营养化的后果。从疏activities活动中释放养分有两种主要方式。第一个原因是挖泥机将泥沙沉积在海湾中作为处置选择时,孔隙水养分的释放;另一个是去除挖泥机材料时暴露的深层沉积物中养分的直接通量。通过收集塔钦河(泰国)河口的沉积物芯并分析孔隙水中的营养物浓度来估算养分释放过程中的最大养分释放,从而确定养分释放。还对深层沉积物核心部分(模拟暴露的沉积物)进行了通量实验,以检查24小时内养分释放的变化。结果表明,氨的初始通量极高,随表面沉积物通量的增加而迅速下降。尽管孔隙水中的磷酸盐浓度很高,但硫化铁矿物的高沉积物氧化速率导致磷酸盐的释放量最小。

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