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首页> 外文期刊>Journal of Hydrology >Spatial variability of chloride deposition in a vegetated coastal area: Implications for groundwater recharge estimation
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Spatial variability of chloride deposition in a vegetated coastal area: Implications for groundwater recharge estimation

机译:植被繁茂的沿海地区氯化物沉积的空间变异性:对地下水补给量的估计

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Knowledge of atmospheric chloride deposition is a prerequisite for applying the chloride mass balance (CMB) method for groundwater recharge estimation. Compared to bare areas, vegetated areas can significantly enhance chloride deposition rates as the vegetation canopy provides a large surface onto which water droplets and aerosols settle. Although generally acknowledged, this effect has often been ignored in practical applications of the CMB method. This paper studies the variability of chloride deposition in a coastal basin characterised by a heterogeneous vegetation cover, and the implications of this variability for groundwater recharge estimation using observation wells in the saturated zone. The study area is located on the Eyre Peninsula in South Australia. The theory of the CMB method for groundwater recharge estimation is revised in the context of highly spatially variable chloride deposition. A GIS-based approach is developed for mapping the chloride deposition accounting for distance from the coast, distribution of vegetation and edge effects; the latter implying a lower chloride deposition inside a vegetation stand than at the edge. In order to quantify the significance of one or several of these effects for recharge estimation, different chloride deposition maps and corresponding recharge estimates are derived. Compared with the reference scenario that accounts for all effects, neglecting the coastal effect results in a 33-36% higher average recharge estimate, whereas neglecting the vegetation effect results in a 17-22% lower average recharge estimate. The latter numbers are likely to represent a lower bound of the impact of neglecting the vegetation effect. A critical factor for accurate determination of the influence of vegetation appears to be the edge effect, albeit its importance is subject to significant uncertainty that warrants further monitoring. (C) 2014 Elsevier B.V. All rights reserved.
机译:了解大气中的氯化物沉积是应用氯离子质量平衡(CMB)方法估算地下水补给量的前提条件。与裸露的地区相比,植被区可以显着提高氯化物的沉积速率,因为植被的冠层提供了较大的表面,水滴和气溶胶可以在其上沉降。尽管已被普遍认可,但这种效果在CMB方法的实际应用中经常被忽略。本文研究了以植被异质覆盖为特征的沿海盆地氯化物沉积的变化性,以及这种变化性对使用饱和带观测井估算地下水补给量的意义。研究区域位于南澳大利亚的艾尔半岛上。 CMB方法用于地下水补给估算的理论在高度空间变化的氯化物沉积的背景下进行了修订。已开发出一种基于GIS的方法来绘制氯化物沉积图,以说明距海岸的距离,植被分布和边缘效应。后者意味着植被内部的氯化物沉积量比边缘处的氯化物沉积量低。为了量化这些效应中的一种或几种对补给估算的重要性,得出了不同的氯化物沉积图和相应的补给估算。与考虑所有影响的参考情景相比,忽略沿海影响会导致平均补给估算值提高33-36%,而忽略植被影响会导致平均补给估算值降低17-22%。后面的数字可能代表了忽略植被效应影响的下限。精确确定植被影响的一个关键因素似乎是边缘效应,尽管其重要性受到重大不确定性的影响,需要进一步监测。 (C)2014 Elsevier B.V.保留所有权利。

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