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首页> 外文期刊>Journal of Hydrology >Impact of various surface covers on water and thermal regime of Technosol
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Impact of various surface covers on water and thermal regime of Technosol

机译:各种表面覆盖物对Technosol的水和热状况的影响

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Different soil covers influence water and thermal regimes in soils within urban areas. Knowledge of these regimes is needed, particularly when assessing effectiveness of energy gathering from soils using horizontal ground heat exchangers. The goal of this study was to calibrate the model HYDRUS-1D for simulating coupled water and thermal regime in Technosol type soils with grass cover, and to use this model for predicting water and thermal regimes under different materials covering the soil surface. For this purpose soil water contents were measured at depths of 10, 20, 30, 40, 60 and 100 cm at 4 locations and temperatures were measured at depths of 20, 40, 80, 120, 150 and 180 cm at three locations (all covered by grass) from June 2011 to December 2012. In addition sensors for simultaneous measuring soil water contents and temperatures were installed under different soil covers (grass, bark chips, sand, basalt gravel and concrete paving) at a depth of 7. The parameters of soil hydraulic properties were obtained on the 100-cm(3) undisturbed soil samples using the multi-step outflow experiment and numerical inversion of the measured transient flow data using HYDRUS-1D. HYDRUS-1D was then used to simulated the water regime within the soil profile under the grass cover using climatic data from June 2011 to December 2012 and some of the soil hydraulic parameters were additionally numerically optimized using soil water contents measured at all depths. Water flow and heat transport were then simulated using these parameters, measured thermal properties and temperatures measured close to the surface applied as a top boundary condition. Simulated temperatures at all depths successfully approximated the measured data.
机译:不同的土壤覆盖率会影响市区内土壤的水和热状况。需要了解这些制度,特别是在评估使用水平地面热交换器从土壤中收集的能量的有效性时。这项研究的目的是校准模型HYDRUS-1D,以模拟Technosol型草覆盖土壤中水与热的耦合,并使用该模型预测覆盖土壤表面的不同材料下的水与热的耦合。为此,在4个位置的10、20、30、40、60和100厘米深度处测量土壤水分,并在三个位置的20、40、80、120、150和180厘米深度处测量温度(所有从2011年6月至2012年12月。此外,在不同深度的土壤覆盖物(草,树皮碎片,沙子,玄武岩碎石和混凝土铺路)下安装了用于同时测量土壤水分和温度的传感器,深度为7。使用多步流出实验在100-cm(3)不变的土壤样品上获得土壤水力学特性,并使用HYDRUS-1D对测得的瞬时流量数据进行数值反演。然后使用HYDRUS-1D利用2011年6月至2012年12月的气候数据模拟草皮下土壤剖面内的水分状况,并使用在各个深度测得的土壤含水量对一些土壤水力参数进行了数值优化。然后使用这些参数模拟水的流动和传热,将测得的热性能和温度测量为接近表面的顶部边界条件。所有深度的模拟温度均成功地逼近了测量数据。

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