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郭涛, 李富春, 陈彦州, 李华仙. 不同岩体交叉裂隙结构下滴状流的分流机理研究[J]. 岩土工程学报. DOI: 10.11779/CJGE20241033
引用本文: 郭涛, 李富春, 陈彦州, 李华仙. 不同岩体交叉裂隙结构下滴状流的分流机理研究[J]. 岩土工程学报. DOI: 10.11779/CJGE20241033
Study on the Diversion Mechanism of Drip flow in Different Rock Mass Intersection Fracture Structures[J]. Chinese Journal of Geotechnical Engineering. DOI: 10.11779/CJGE20241033
Citation: Study on the Diversion Mechanism of Drip flow in Different Rock Mass Intersection Fracture Structures[J]. Chinese Journal of Geotechnical Engineering. DOI: 10.11779/CJGE20241033

不同岩体交叉裂隙结构下滴状流的分流机理研究

Study on the Diversion Mechanism of Drip flow in Different Rock Mass Intersection Fracture Structures

  • 摘要: 岩土体中存在由大量天然裂隙组成的复杂且庞大的裂隙结构,地表积水沿裂隙下渗将引起岩土体力学性质改变。由于交叉裂隙对于非饱和裂隙结构渗流起重要控制作用,该文采用相场方法模拟两相界面,对不同几何结构的交叉裂隙中滴状流进行了计算。探讨了交叉裂隙的几何结构(开度比、倾斜角、裂隙夹角等)对于液滴在裂隙交叉口处分流行为的影响,并结合XGBoost方法对几何结构的三个参数进行了特征重要性分析。结果表明:通过与文献实验结果对比,验证了该计算方法的准确性和有效性;液滴在裂隙交叉口处表现出完全分流、部分分流且无拖曳现象、部分分流有拖曳现象、不分流4种流动形态;随着裂隙开度比 、裂隙整体与水平面夹角 及裂隙间夹角 的增大,液滴的分流比例 在减小甚至出现不分流现象;特别的当液滴长度为2 cm时,在 时出现明显的拖曳现象、 时液滴完全分流进入另一通道、当 时,液滴在到达交叉口处时将不在流动,被储存在裂隙中;通过特征重要性分析,发现裂隙整体与水平面夹角 和裂隙间夹角 对于液滴分流行为的影响远高于裂隙开度比 。将此计算模型推广至裂隙网络结构中,对自然界中地表积水在裂隙结构中的非饱和渗流进行了模拟。发现裂隙结构中常出现由于裂隙内空气的“阻塞效应”引起的不饱和流动现象,液滴在其中选择的“优势通道”与出入口间通道的笔直程度、过流面积等因素密切相关。其结果可为工程中随机裂隙、裂隙结构的渗流仿真和工程设计提供一定的理论分析基础和方法借鉴。

     

    Abstract: There is a complex and huge fracture network composed of a large number of natural fractures in the rock and soil body, and surface water seepage along the cracks will cause the change of physical properties of rock and soil. In this paper, the phase field method is used to simulate the two-phase interface, and the finite element method is used to simulate the drip flow in the intersecting fracture network with different geometric structures. The paper explores the influence of the geometric structure of cross fractures (fracture width ratio, inclination angle, crack angle, etc.) on the split-flow behavior of droplets at the intersection. Additionally, the XGBoost method is used to conduct the feature importance analysis with three parameters of the geometric structure. The results indicate that: by comparing with experimental results from the literature, the accuracy and effectiveness of the computational method are verified; droplets at the fracture intersection exhibit four flow patterns: complete diversion, partial diversion without drag, partial diversion with drag, and no diversion; as the fracture width ratio( ), the overall angle between the fracture and the horizontal plane, and the angle between fractures increase, the diversion ratio( ) of the droplets decreases and may even result in no diversion; particularly, when the droplet length is 2 cm, a significant drag phenomenon occurs at , droplets completely divert into another channel at , and at , droplets cease to flow upon reaching the intersection and are stored in the fracture; through feature importance analysis, it is found that the overall angle between the fracture and the horizontal plane and the angle between fractures have a much greater impact on the diversion behavior of droplets than the fracture width ratio( ). Extending this computational model to a network of fractures, the model simulates the unsaturated seepage in surface water accumulation within fracture structures in nature. It is found that unsaturated flow phenomena often occur in fracture structures due to the "blocking effect" of air within the fractures, and the "dominant channels" chosen by droplets are closely related to the straightness of the channels between the inlet and outlet and the flow area. The results can provide a theoretical analysis foundation and methodological reference for the seepage simulation and engineering design of random fractures and fracture structures in engineering.

     

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