利用WEPP模型模拟东地中海生态系统当前和未来的径流和土壤侵蚀动态

IF 8 Q1 ENERGY & FUELS
Safwan Mohammed
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引用次数: 0

摘要

径流(RF)和土壤侵蚀(SE)对环境系统有负面影响,既有现场效应,也有场外效应。本研究旨在评估水侵蚀预测项目(WEPP)模型在四个地点预测SE和RF的性能,这些地点代表三个生态系统:农业用地(位置- ks坡度为8%,位置- mn坡度为20%),森林(位置- ainf坡度为35%)和烧毁森林(位置- ainbf坡度为35%)。预测了未来20年生态系统对SE和RF的响应。该研究于2019年至2038年在地中海东部进行,2019年作为参考年,将WEPP模型输出与研究地点的实测值进行比较。模型性能指标表明WEPP模型在预测SE(模型效率(NSE) =0.67,决定系数(R2) =0.97)和RF (NSE=0.66, R2=0.78)方面具有适用性。未来预测表明,农业生态系统在SE和RF方面优于其他生态系统。但是,年度RF可排序如下:KS (234.7mm±75.6)>;MN(141.1毫米±50.2)比;AINF (145.4mm±47.4)>;AINBF(100.3毫米±49.2)。同样,SE可分为:KS (2.38 kg/m2±1.36)>;AINF (0.45 kg/m2±0.17)>;MN (0.31 kg/m2±0.11)>;AINBF (0.24 kg/m2±0.15)。然而,月均的SE和RF结果在KS区域更为明显,而在其他生态系统则不太明显。土壤含水量(θ, %)和土壤水导率(Ksw, mm/hr)在夏季(6 ~ 8月)θ值最低,分别为KS、MN、AINF和AINBF的46.3%、50.3%、46.2%和49.2%。相反,最高的Ksw预测在夏季,在3.3至6.3毫米/小时之间。本研究促进了将WEEP模型作为地中海东部生态系统管理的可持续工具,帮助决策者进行恢复规划。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Modeling current and future run-off and soil erosion dynamics in Eastern Mediterranean ecosystems using the WEPP model

Modeling current and future run-off and soil erosion dynamics in Eastern Mediterranean ecosystems using the WEPP model
Run-off (RF) and soil erosion (SE) have a negative impact on the environmental system, with both on-site and off-site effects. This research aimed to evaluate the performance of the Water Erosion Prediction Project (WEPP) model in predicting SE and RF across four locations representing three ecosystems: agricultural land (location-KS at 8 % slope, location-MN at 20 % slope), forest (location-AINF at 35 % slope), and burned forest (location-AINBF at 35 % slope). It also predicts the future responses of the studied ecosystems to SE and RF for the upcoming 20 years. The study was conducted in the eastern Mediterranean from 2019 to 2038, 2019 served as the reference year to compare WEPP model output with measured values at the studied locations. Model performance indicators showed the applicability of WEPP model in predicting SE (model efficiency (NSE) =0.67, coefficient of determination (R2) =0.97), RF (NSE=0.66, R2=0.78). Future projections revealed that the agricultural ecosystem exceeded others in terms of SE and RF. However, annual RF can be ranked as follows: KS (234.7mm±75.6)> MN (141.1mm±50.2)> AINF (145.4mm±47.4) > AINBF (100.3mm±49.2). Similarly, SE can be classified as: KS (2.38 kg/m2 ±1.36)> AINF (0.45 kg/m2 ±0.17) > MN (0.31 kg/m2 ±0.11)> AINBF (0.24 kg/m2 ±0.15). However, monthly results of SE and RF were more intense in the KS location and less pronounced in the rest of the ecosystems. An analysis of associated factors, namely, soil water content (θ, %), and soil water hydraulic conductivity (Ksw, mm/hr), revealed the lowest θ values occurred during the summer season (June to August), reaching 46.3 %, 50.3 %, 46.2 %, and 49.2 %, for KS, MN, AINF, and AINBF, respectively. Conversely, the highest Ksw was forecasted in summer, ranging from 3.3 to 6.3 mm/hr. This research promotes utilizing the WEEP model as a sustainable tool for ecosystem management in the eastern Mediterranean, aiding decision-makers in rehabilitation planning.
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来源期刊
Energy nexus
Energy nexus Energy (General), Ecological Modelling, Renewable Energy, Sustainability and the Environment, Water Science and Technology, Agricultural and Biological Sciences (General)
CiteScore
7.70
自引率
0.00%
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0
审稿时长
109 days
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