S. Gopinath, K. Srinivasamoorthy, R. Prakash , A. Rajesh Kanna, V. Gopalakrishnan
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引用次数: 0
摘要
海底地下水排放(SGD)将大量营养物质从内陆输送到海洋。尽管如此,在孟加拉湾泰米尔纳德邦的Cuddalore海岸,与SGD相关的营养物质通量一直没有被注意到,暴露在深思熟虑的环境问题中。目前的尝试是评估SGD辅助的氡和养分通量。采集地下水样本,分析pH值、电导率、总溶解固体、盐度、氡、氮、磷和二氧化硅。地下水样品中的氡含量在0.1至7.9之间,平均值为2.2 Bq L−1。根据氡质量平衡计算的SGD通量范围为0.11至15.03,平均为3.42 m d−1。溶解无机氮、溶解无机磷酸盐和溶解二氧化硅的SGD相关溶解营养素分别为4292.0、184.0和1442.2µmol L−1 d−1。SGD的数量和伴随的养分通量受到降水、水力梯度和含水层环境(如缺氧和缺氧)的影响。
An investigation of submarine groundwater discharge and related fluxes in parts of the southeast coast of India: Combined radon and nutrients mass balance approach
Submarine groundwater discharge (SGD) delivers significant nutrients from inland to oceans. Nevertheless, SGD-related nutrient fluxes have been unnoticed in the Cuddalore coast of Tamil Nadu, Bay of Bengal, exposed to thoughtful environmental issues. The present attempt was to assess SGD-aided radon and nutrient fluxes. Groundwater samples were collected and analyzed for pH, electrical conductivity, total dissolved solids, salinity, radon, nitrogen, phosphorous, and silica. The radon in groundwater samples lies between 0.1 and 7.9, with an average of 2.2 Bq L−1. The SGD flux calculated from radon mass balance ranges from 0.11 to 15.03, with an average of 3.42 m d−1. The SGD-associated dissolved nutrients were 4292.0, 184.0, and 1442.2 µ mol L−1 d−1 for dissolved inorganic nitrogen, dissolved inorganic phosphate, and dissolved silica, respectively. The quantum of SGD and accompanying nutrient fluxes were prejudiced by precipitation, hydraulic gradient, and aquifer environments like oxic and anoxic.