三维虚拟石质土有效水力特性反演方法研究

4区 农林科学 Q2 Agricultural and Biological Sciences Soil Science Pub Date : 2021-09-24 DOI:10.5194/soil-2021-99
M. Naseri, S. Iden, W. Durner
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引用次数: 4

摘要

摘要含有大量岩石碎片的石质土壤在世界各地广泛存在。然而,确定石质土(SHP)有效水力特性的实验,即水保持曲线(WRC)和水力传导曲线(HCC),具有挑战性。在这些土壤中安装测量装置和传感器是困难的,而且由于高度的局部异质性,数据不太可靠。因此,石质土特别是非饱和水力条件下的有效特性仍未得到很好的了解。另一种评估具有内部结构非均匀性的系统的SHP的方法是数值模拟。我们使用Hydrus 2D/3D软件在3D中创建虚拟石质土壤,并模拟不同体积岩石碎片含量的水流。f.通过在砂壤土中放置岩石碎片形式的不透水球体,创建了体积岩石含量为11%至37%的土壤。在虚拟蒸发实验中生成了不同深度的局部压头、平均含水量和上边界通量的时间序列。此外,采用多步单元梯度模拟来确定pF = 2附近的水力导电性有效值。假设系统为均匀系统,通过反建模对生成的数据进行评估,并确定有效水力特性。对不同体积岩石破碎块的有效特性与现有SHP标度模型的预测结果进行了比较。我们的研究结果表明,在不透水岩石碎片的情况下,仅基于f值缩放背景土的WRC给出了可接受的结果。然而,电导率的降低不能简单地通过f的值来衡量。通过应用Novák、Maxwell和GEM模型来衡量HCC,预测得到了极大的提高。Maxwell模型与数值识别的HCC最吻合。
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Effective hydraulic properties of 3D virtual stony soils identified by inverse modeling
Abstract. Stony soils that have a considerable amount of rock fragments are widespread around the world. However, experiments to determine effective hydraulic properties of stony soils (SHP), i.e. the water retention curve (WRC) and hydraulic conductivity curve (HCC), are challenging. Installation of measurement devices and sensors in these soils is difficult and the data are less reliable because of high local heterogeneity. Therefore, effective properties of stony soils especially in unsaturated hydraulic conditions are still not well understood. An alternative approach to evaluate the SHP of these systems with internal structural heterogeneity is numerical simulation. We used the Hydrus 2D/3D software to create virtual stony soils in 3D and simulate water flow for different volumetric rock fragment contents, f. Soils with volumetric stone contents from 11 to 37 % were created by placing impermeable spheres in the form of rock fragments in a sandy loam soil. Time series of local pressure heads in various depths, mean water contents and fluxes across the upper boundary were generated in a virtual evaporation experiment. Additionally, a multi-step unit gradient simulation was applied to determine effective values of hydraulic conductivity near saturation up to pF = 2. The generated data were evaluated by inverse modeling, assuming a homogeneous system, and the effective hydraulic properties were identified. The effective properties were compared with predictions from available scaling models of SHP for different volumes of rock fragments. Our results showed that scaling the WRC of the background soil based on only the value of f gives acceptable results in the case of impermeable rock fragments. However, the reduction of conductivity could not be simply scaled by the value of f. Predictions were highly improved by applying the Novák, Maxwell, and GEM models to scale the HCC. The Maxwell model matched the numerically identified HCC best.
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来源期刊
Soil Science
Soil Science 农林科学-土壤科学
CiteScore
2.70
自引率
0.00%
发文量
0
审稿时长
4.4 months
期刊介绍: Cessation.Soil Science satisfies the professional needs of all scientists and laboratory personnel involved in soil and plant research by publishing primary research reports and critical reviews of basic and applied soil science, especially as it relates to soil and plant studies and general environmental soil science. Each month, Soil Science presents authoritative research articles from an impressive array of discipline: soil chemistry and biochemistry, physics, fertility and nutrition, soil genesis and morphology, soil microbiology and mineralogy. Of immediate relevance to soil scientists-both industrial and academic-this unique publication also has long-range value for agronomists and environmental scientists.
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