首页> 外文期刊>Journal of arid environments >GIS-based hydrological modelling to assess runoff yields in ancient- agricultural terraced wadi fields (central Negev desert)
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GIS-based hydrological modelling to assess runoff yields in ancient- agricultural terraced wadi fields (central Negev desert)

机译:基于GIS的水文模型来评估古代农业梯田旱谷田(内盖夫中部沙漠)的径流产量

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Thousands of ancient agricultural terraced fields exist in ephemeral stream valleys in the central Negev desert. Their stone terrace walls captured runoff water, flowing from the surrounding hillslope catchments, to increase moisture in the loess soils of the terraced fields. Geoarchaeological research at the site of Horvat Haluqim discovered evidence for ancient farming and soil manuring in this arid desert region during various archaeological periods. Geographic Information Systems (GIS) and Digital Elevation Models (DEM) enable the development of hydrological models to investigate every ancient terraced field in a non-invasive manner, without disturbing the archaeological remains We developed a GIS-based hydrological model, coupled with the D Infinity (Tau DEM) algorithm, to evaluate annual runoff yields in 13 ancient terraced fields at the rural archaeological site of Horvat Haluqim. Our model precisely determined the runoff catchment area, ranging between 0.10 ha and 0.36 ha, of each individual terraced field. Supervised land cover classification, using Erdas Imagine, showed the surface percentages of crusted loess soil and exposed bedrock. Following an evaluation of runoff coefficients established by conventional hydrological studies in the region, we present results of model calculated runoff overland flow yields. We modelled runoff amounts for each of the agricultural fields during an average year (1989-90) with 88 mm precipitation, a very wet year (1991-92) with 188 mm, and a severe drought year (1999-2000) with only 34 mm rainfall. Our initial results, based on an approximated average annual runoff coefficient of 10%, indicate that runoff water amounts during an average and wet rainfall year appear sufficient to grow agricultural crops in these ancient fields. However, drought years are of course more problematic. The modelling results are supported by the successful growth of trees in similar terraced wadi fields next to Horvat Haluqim, established by the Jewish National Fund. Given the inherent uncertainties involved in modelling, it is encouraging to note that the trees did survive also drought years. Our model may be applied to evaluate the effect of climatic changes on runoff water harvesting systems, looking back into the past and also to assess possible impact of future climate change scenarios in modern water harvesting projects.
机译:内盖夫沙漠中部的短暂河谷中有成千上万的古老农业梯田。他们的石质梯田墙捕获了从周围的山坡集水区流出的径流水,以增加梯田的黄土土壤中的水分。 Horvat Haluqim遗址的地质考古研究发现了在这个干旱沙漠地区各个考古时期的古代耕作和土壤耕作的证据。地理信息系统(GIS)和数字高程模型(DEM)使水文模型的开发能够以非侵入性的方式调查每个古代梯田,而不会干扰考古遗迹。我们开发了基于GIS的水文模型,并结合了D Infinity(Tau DEM)算法,用于评估Horvat Haluqim农村考古现场13个古老梯田的年径流量。我们的模型精确地确定了每个梯田的径流集水面积,范围在0.10公顷至0.36公顷之间。使用Erdas Imagine进行的有监督的土地覆被分类显示了硬皮黄土和裸露的基岩的表面百分比。在对该地区常规水文研究确定的径流系数进行评估之后,我们介绍了模型计算的径流陆上径流产量的结果。我们对每个农业田的平均年径流量(1989-90年)进行了建模,降水量为88毫米,非常潮湿的年份(1991-92年)为188毫米,严重干旱的年份(1999-2000年)为34毫米毫米的降雨量。我们基于大约10%的年平均径流系数的初步结果表明,在平均和潮湿的降雨年中,径流水量似乎足以在这些古代土地上种植农作物。但是,干旱年当然更成问题。建模的结果得到了犹太国家基金会建立的Horvat Haluqim旁类似梯田旱田中树木成功生长的支持。考虑到建模所固有的不确定性,令人鼓舞的是,这些树木确实可以在干旱年份生存下来。我们的模型可以用于评估气候变化对径流集水系统的影响,回顾过去,还可以评估未来气候变化情景在现代集水项目中可能产生的影响。

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