Reda Yonas, Moges Awdenegest, Kendie Hailu
Sekota Dry-land Agricultural Research Center, Soil and Water Management Research, P.O. Box 62, Sekota, Ethiopia.
Hawassa University, Institute of Technology, P.O. Box 05, Hawassa, Ethiopia.
Heliyon. 2024 Jul 25;10(15):e35052. doi: 10.1016/j.heliyon.2024.e35052. eCollection 2024 Aug 15.
The study utilized the Modified Universal Soil Loss Equation (MUSLE) to predict sediment loss and evaluate the model's performance in the Agewmariam experimental watershed in order to support the planning, management, and appropriate use of the soil and water resources in the watershed. The natural resources conservation service (NRCS) curve number method was used to model runoff energy factor. By overlaying maps of runoff energy, soil erodibility, slope length and steepness, cover management, and support practice factors with assigned values, the cumulative effect of these parameters for the suspended sediment yield was calculated using the ArcGIS raster calculator. The runoff energy factor was the most sensitive parameter, followed by slope length and steepness factor. To improve the model's fit to the local conditions, the initial abstraction to storage ratio (λ) of the runoff energy factor was reduced to 0.023, and the MUSLE model coefficient and exponent were adjusted to 1 and 0.59, respectively. During calibration, the mean observed and estimated suspended sediment yields were 0.2 and 0.23 ton/ha, respectively, while during validation, they were 0.7 and 0.53 ton/ha, respectively. The model evaluation showed that the MUSLE model, without calibration, was not appropriate for estimating runoff and sediment yield. However, with appropriate calibration, the model showed good performance with a coefficient of determination (R), coefficient of efficiency (E), and index of agreement (d) of 0.85, 0.85, and 0.96 respectively, during calibration and 0.84, 0.65, and 0.83 respectively, during validation. Based on these findings, this study suggests that the calibrated MUSLE model can be used to prioritize soil and water conservation interventions within the watershed or can be extrapolated to neighboring similar watersheds. Further refinement of model input parameters using more data from the watershed is recommended to increase the prediction accuracy of the model.
该研究利用修正通用土壤流失方程(MUSLE)预测沉积物流失,并评估该模型在阿格韦马里亚姆实验流域的性能,以支持该流域土壤和水资源的规划、管理及合理利用。采用自然资源保护局(NRCS)曲线数法对径流能量因子进行建模。通过将径流能量、土壤可蚀性、坡长和坡度、植被覆盖管理及支撑实践因子的地图与指定值叠加,利用ArcGIS栅格计算器计算这些参数对悬浮泥沙产量的累积影响。径流能量因子是最敏感的参数,其次是坡长和坡度因子。为提高模型对当地条件的拟合度,将径流能量因子的初始入渗蓄存比(λ)降至0.023,并将MUSLE模型系数和指数分别调整为1和0.59。在校准期间,观测到的和估计的悬浮泥沙产量均值分别为0.2和0.23吨/公顷,而在验证期间,它们分别为0.7和0.53吨/公顷。模型评估表明,未经校准的MUSLE模型不适用于估算径流和泥沙产量。然而,经过适当校准后,该模型在校准期间的决定系数(R)、效率系数(E)和一致性指数(d)分别为0.85、0.85和0.96,在验证期间分别为0.84、0.65和0.83,表现良好。基于这些发现,本研究表明,校准后的MUSLE模型可用于确定该流域内水土保持干预措施的优先级,或可外推至邻近的类似流域。建议利用该流域更多数据进一步优化模型输入参数,以提高模型的预测精度。