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Vadose Zone Transport of Nitrate in the Sierra Pelona Groundwater Basin, Agua Dulce, California

机译:加利福尼亚州阿瓜杜尔塞山脉Pelona地下水盆地中硝酸盐的渗流区运输

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Using data from previous studies about nitrate contamination in Agua Dulce, CA andthe numerical modeling program HYDRUS-1D, nitrate transport in the vadose zoneassociated with septic system discharges was evaluated. Thirty-six modelingscenarios were assessed and the results analyzed. With soil borings less than 6 mdeep, steady state nitrate transport within the system is reached within 200 days,while steady state is not reached with the deeper boring within 500 days. Themodeling results show that the nitrate concentration plume is less than the maximumcontaminant level (MCL) of 10 mg/L within 1.3 m below the septic leachfield in allscenarios. The analysis of the fully-mixed tank scenario clearly shows that nitrateconcentrations in groundwater are of greater concern during drought conditions.These findings help explain the pattern of nitrate concentrations observed in theaquifer system in this region.
机译:使用先前关于加利福尼亚州阿瓜·杜尔塞和加利福尼亚州硝酸盐污染的研究数据 HYDRUS-1D数值建模程序,渗流带中的硝酸盐迁移 对与化粪池系统排放有关的疾病进行了评估。三十六建模 评估情景并分析结果。土壤钻孔小于6 m 在200天内达到了系统内深层,稳态​​硝酸盐的传输, 而500天之内的更深层次的沉闷并没有达到稳定状态。这 模拟结果表明,硝酸盐浓度羽流小于最大浓度。 在所有化粪池浸出场以下1.3 m内的污染物水平(MCL)为10 mg / L 场景。对全混罐情景的分析清楚地表明,硝酸盐 在干旱条件下,地下水中的浓度更加令人关注。 这些发现有助于解释观察到的硝酸盐浓度的模式。 该区域的含水层系统。

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