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Examples of water flow simulations in simple and complex (Mallants et al., 1999) capillary barriers. Download now (3.4 MB)
Grignon Numerical analysis of water and solute transport in a cultivated silt loam soil (heterogeneity generated by farming practices) (Coquet et al., 2005).
This web site offers many other tools that may be helpful especially for beginning HYDRUS users. We continue to provide the Frequently Asked Questions (FAQ) and Discussion Forums where users can obtain answers to most of the more common questions as well as be able to share their experience, pose questions, and seek guidance for specific applications. We will continue to actively support these tools. You can also view simple demos (for Version 1 and Version 2) that illustrate the use of the new HYDRUS software, accompanied with brief explanations of particular commands and actions. Additionally, we provide a list of references so that potential HYDRUS users can see additional examples, in which HYDRUS has been applied in the past, and existing users can find help with their own applications.
HYDRUS可用来分析水质和溶质在非饱和、部分饱和或是饱和多孔介质情况下的运动。HYDRUS可由不规则边界处理水流区域,水流区域本身可能是由非均匀土壤组成具有局部各向任意程度。水流和运移可能发生在垂直面,也可能在水平面,具有径向对称性的垂直轴或三维区域。
模型的水流部分可以用来处理连续或时变的规定的方向和流量边界,以及由气象条件控制的边界。土壤表面边界条件在模拟从给定的流量到规定的方向类型条件期间可能会发生变化,反之亦然。它还可以通过水域饱和部分的剩余水量和不排水边界条件处理自由面边界。节点排水是由一个简单的模拟实验关系为代表。
对溶质运移来说,软件既支持连续和变化的规定浓度(Dirichlet或first-type)也支持浓度通量边界(Cauchy或third-type)。弥散张量包含分子扩散和曲折的结果反应影响。
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Examples of water flow and solute transport simulations in a randomly generated stochastic field of scaling factors representing soil heterogeneity. Download now (1.3 MB)
Floods Examples of water flow simulations in a flood plain. Examples demonstrate the use of dynamic time-dependent boundary conditions.
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