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的水文建模,以评估古代农业梯田瓦迪领域的径流产量(中央Negev沙漠)

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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:在Neeve Darder中央山谷中,成千上万的古代农业露台领域存在于短期谷物中。他们的石头露台墙壁捕获了径流水,从周围的山坡流量流动,从而增加露台的黄土水域中的水分。在各种考古时期,Horvat Haluqim遗址Horvat Haluqim网站发现了这个干旱沙漠地区古农业和土壤的证据。地理信息系统(GIS)和数字海拔模型(DEM)使水文模型的发展能够以非侵入性的方式调查每个古老的露台领域,而不会扰乱考古学仍然是我们开发了一种基于GIS的水文模型,加上D Infinity(TAU DEM)算法,评估Horvat Haluqim农村考古遗址13个古老露台的年径流产量。我们的模型精确地确定了径流集水区,每个单独的露台场的0.10公顷和0.36公顷。监督土地覆盖分类,使用Erdas Imagine,显示出裂纹黄土土壤和暴露基岩的表面百分比。在该地区确定的常规水文研究建立的径流系数进行评估之后,我们呈现了模型计算径流覆盖流量的结果。我们在平均年(1989-90)中为每一个农业领域建模径流金额,其中88毫米降水,一个非常潮湿的年(1991-92),188毫米,并且仅为34岁的严重干旱年份(1999-2000)毫米降雨。我们的初始结果基于近似平均年径流系数10%,表明平均和潮湿的降雨年度的径流水量似乎足以在这些古老的领域种植农业作物。然而,干旱岁语当然更有问题。由犹太国家基金建立的Horvat Haluqim旁边的类似梯田瓦迪领域的树木成功增长的建模结果支持。鉴于建模中所涉及的固有的不确定性,令人鼓舞的是,树木确实生存了趋势。我们的模型可用于评估气候变化对径流液收集系统的影响,回顾过去,并评估未来气候变化情景在现代水收集项目中的可能影响。

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