酸性硫酸盐土壤和酸性排水,浅滩港下游泛滥平原,新南威尔士州

M. Pease, A. Nethery, A. Young
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引用次数: 2

摘要

摘要对新南威尔士州南海岸浅滩滩下贾斯贝尔斯灌木丛酸性硫酸盐土壤区域的地下水位波动和水质进行了为期8个月的调查。在一个大型主要防洪排水渠的后沼泽样带中分析了地下水位波动,以了解地下水运动及其对酸性排水严重程度的影响。随着地下水位下降,地下水酸度迅速增加,地下水中硫酸盐、铁和铝的浓度升高。还分析了所研究的主要排水管长度的水质。在涨潮时,含盐的溪水流入排水沟,显示出一种中和酸的作用。在一次小洪水事件发生一个月后,对布劳顿溪的水质进行了分析,结果(主要是pH值降低和铝浓度升高)突出了从洪泛区到小溪的酸性排水的运动。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Acid sulfate soils and acid drainage, Lower Shoalhaven floodplain, New South Wales
An eight-month long investigation is reported of watertable fluctuations and water quality in an area of acid sulphate soils at Jaspers Brush, lower Shoalhaven floodplain, south coast of NSW. Watertable fluctuations were analysed in a backswamp transect across a large main flood mitigation drain to understand groundwater movement and its influence on the severity of acid drainage. As the watertable dropped, groundwater acidity increased rapidly and sulphate, iron and aluminium concentrations in groundwater rose to elevated concentrations. Water quality was also analysed along the length of the main drain studied. The influx of saline creek waters into the drain during high tides was shown to have an acid neutralising effect. Water quality in Broughton Creek was analysed for a month after a minor flood event, with results (mainly lowered pH and elevated aluminium concentrations) highlighting the movement of acid drainage from the floodplain into the creek.
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