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Application of the EGEM model to predict ephemeral gully erosion in Sicily, Italy.

机译:EGEM模型在意大利西西里岛的短暂性沟壑侵蚀预测中的应用。

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Recent research has shown the importance of ephemeral gully (EG) erosion in the context of global erosion and, at the same time, the lack of adequate models to estimate it. At present, the ephemeral gully erosion model (EGEM) is the only conceptual model specifically developed for ephemeral gully erosion estimation. The main aim of the paper is to evaluate the performance of EGEM model adapted to local conditions compared with that of simple empirical equations. A data set of 92 ephemeral gullies formed between 1995 and 2000 in a wheat-cultivated study area in Sicily, Italy, was used for the purpose. In order to improve EGEM performance, two important adaptations were made. Both the rain distribution type and the causative rainfall of the hydrological component of EGEM were modified to reproduce local conditions. The EGEM assumption of a constant depth for the entire length of the ephemeral gully was also modified. EGEM performance was tested with two different rain distribution types, three different causative rainfalls and two different EG depths. The adaptation of the EGEM hydrological component improves the volume prediction with respect to the standard version of EGEM; the improvement is mainly due to the rain distribution type, whereas causative rainfall seems to be less important. The use of adjusted EG depths is, however, essential to minimize the errors between measured and predicted volumes. The capability of EGEM to predict the ephemeral gully cross-section is weak and non-significant relationships were found between measured and estimated width. A regression analysis between ephemeral gully-eroded volume and different morphological, topographical and hydrological parameters confirms the great importance of EG length to explain eroded volume (R2=0.64 for the simple correlation between volume and length). Considering that the adaptation of the hydrological component and the measurement of EG depths are necessary for the EG volumes estimated by EGEM to be reliable, it seems more simple, as suggested by other authors, to use empirical relations between eroded volume and length performed in different environments, until more precise physically based models are developed..
机译:最近的研究表明,在全球侵蚀的背景下,临时性沟壑侵蚀非常重要,与此同时,缺乏足够的模型来估算它。目前,短暂河道侵蚀模型(EGEM)是唯一专门为短暂河道侵蚀评估开发的概念模型。本文的主要目的是与简单的经验方程相比,评估适合当地条件的EGEM模型的性能。为此,使用了1995年至2000年之间在意大利西西里岛一个小麦种植研究区形成的92个临时沟壑的数据集。为了提高EGEM性能,进行了两个重要的修改。修改了EGEM的雨水分布类型和因果降雨,以再现当地条件。 EGEM的假设是短暂的整个沟壑的深度是恒定的。在两种不同的降雨分布类型,三种不同的致雨量和两种不同的EG深度下测试了EGEM性能。相对于EGEM的标准版本,对EGEM水文组件的适应性提高了体积预测;改善主要归因于降雨分布类型,而引起降雨似乎不那么重要。但是,使用调整后的EG深度对于最小化测量体积和预测体积之间的误差至关重要。 EGEM预测短暂沟壑横截面的能力很弱,并且在测量宽度和估计宽度之间发现不显着的关系。临时沟壑侵蚀量与不同形态,地形和水文参数之间的回归分析证实了EG长度对于解释侵蚀量的重要性(R2 = 0.64对于体积和长度之间的简单关系)。考虑到水文分量的适应和EG深度的测量对于EGEM估计的EG量的可靠性是必要的,如其他作者所建议的那样,使用侵蚀量和长度在不同条件下进行的经验关系似乎更为简单。环境,直到开发出更精确的基于物理的模型。

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