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融雪对土壤硝酸盐淋失至地下水的影响——一项模型研究。

Importance of snowmelt on soil nitrate leaching to groundwater - A model study.

作者信息

Beegum Sahila, Malakar Arindam, Ray Chittaranjan, Snow Daniel D

机构信息

Nebraska Water Center, Part of the Robert B. Daugherty Water for Food Global Institute, 2021 Transformation Drive, University of Nebraska, Lincoln, NE 68588-6204, USA; Adaptive Cropping System Laboratory, USDA-ARS, Beltsville, MD 20705, USA.

School of Natural Resources and Nebraska Water Center, Part of the Robert B. Daugherty Water for Food Global Institute, 202 Water Sciences Laboratory, University of Nebraska, Lincoln, NE 68583-0844, USA.

出版信息

J Contam Hydrol. 2023 Apr;255:104163. doi: 10.1016/j.jconhyd.2023.104163. Epub 2023 Feb 16.

Abstract

The movement of nitrate to surface water bodies during snow accumulation and melting has been extensively studied, but there are only limited studies on the influence of snow processes on nitrate leaching to groundwater. The present study investigated the impact of snow processes on nitrate leaching to groundwater based on a simulation modeling approach using HYDRUS-1D. HYDRUS-1D model has a temperature threshold-based snow model in addition to water, solute, and heat simulation components. The snow component in HYDRUS-1D was previously not applied to snow simulation studies since the method does not consider a detailed physical and process-based representation of snow accumulation and melting. In the present study, HYDRUS-1D was used to simulate snow accumulation and melting over 30 years for a location in Waverly, Lancaster County, Nebraska, USA. From the simulations, it was observed that the calibrated temperature threshold based snow module in HYDRUS-1D is effective in simulating snow accumulation and melting, as shown by the index of agreement and root mean squared error of 0.74 and 2.70 cm for calibration (15 years) and 0.88 and 2.70 cm for validation (15 years), respectively. The impact of snow melt on nitrate leaching was studied based on a study area with corn cultivation (Waverly, Nebraska, USA). A long-term (60 years) analysis was carried out for irrigated and non-irrigated agriculture with and without precipitation as snow. A higher nitrate leaching to groundwater was observed in the order of irrigated-with snow (54,038 kg/ha), irrigated-without snow (53,516 kg/ha), non-irrigated-with snow (7,431 kg/ha), and non-irrigated-without snow (7,090 kg/ha). This displays a 0.98% and 4.81% increase in nitrate leaching due to snow in irrigated and non-irrigated conditions, respectively. When extrapolated over the corn cultivated regions in Nebraska, this resulted in a difference of 1.2E+09 kg and 6.1E+08 kg of nitrate when considering snow in irrigated and non-irrigated areas over 60 years. This is the first study that has analyzed the long-term impact of snow on nitrate transport to groundwater based on a simulation modeling approach. The results show that snow accumulation and melting plays a vital role in the nitrate leaching into the groundwater and indicates the importance of considering snow components in similar studies.

摘要

在积雪和融雪过程中硝酸盐向地表水体的迁移已得到广泛研究,但关于积雪过程对硝酸盐淋溶至地下水的影响的研究却十分有限。本研究基于使用HYDRUS - 1D的模拟建模方法,调查了积雪过程对硝酸盐淋溶至地下水的影响。HYDRUS - 1D模型除了具备水、溶质和热量模拟组件外,还有一个基于温度阈值的积雪模型。HYDRUS - 1D中的积雪组件此前未应用于积雪模拟研究,因为该方法没有考虑积雪和融雪基于详细物理过程的表征。在本研究中,使用HYDRUS - 1D对美国内布拉斯加州兰卡斯特县韦弗利一处地点30年的积雪和融雪情况进行了模拟。从模拟结果可以看出,HYDRUS - 1D中经过校准的基于温度阈值的积雪模块在模拟积雪和融雪方面是有效的,校准(15年)时的一致性指数和均方根误差分别为0.74和2.70厘米,验证(15年)时分别为0.88和2.70厘米。基于美国内布拉斯加州韦弗利玉米种植区的研究区域,研究了融雪对硝酸盐淋溶的影响。对有灌溉和无灌溉的农业,以及有降雪和无降雪情况下进行了为期60年的长期分析。观察到硝酸盐向地下水的淋溶量从高到低依次为:有灌溉且有降雪(54,038千克/公顷)、有灌溉但无降雪(53,516千克/公顷)、无灌溉且有降雪(7,431千克/公顷)、无灌溉且无降雪(7,090千克/公顷)。这表明在有灌溉和无灌溉条件下,由于降雪导致的硝酸盐淋溶量分别增加了0.98%和4.81%。当将此结果外推至内布拉斯加州的玉米种植区时,考虑60年中有灌溉和无灌溉地区的降雪情况,硝酸盐淋溶量的差异分别为1.2E + 09千克和6.1E + 08千克。这是第一项基于模拟建模方法分析积雪对硝酸盐向地下水迁移的长期影响的研究。结果表明,积雪和融雪在硝酸盐淋溶至地下水中起着至关重要的作用,并表明在类似研究中考虑积雪组件的重要性。

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