关于研究地下水运动的方法探讨  

Discussion on methods of studying groundwater movement

作　　者：郭倩 王超 都兰 Guo Qian;Wang Chao;Du Lan(Inner Mongolia Huankeyuan Environmental Technology Co.,Ltd,Hohhot Inner Mongolia 010011,China;Inner Mongolia Ecological Environment Scientific Research Institute Co.,Ltd,Hohhot Inner Mongolia 010011,China;Inner Mongolia Institute of Environmental Science,Hohhot Inner Mongolia 010011,China)

机构地区：[1]内蒙古环科园环境科技有限责任公司,呼和浩特010011 [2]内蒙古生态环境科学研究院有限公司,呼和浩特010011 [3]内蒙古自治区环境科学研究院,呼和浩特010011

出　　处：《环境与发展》2021年第2期125-128,共4页Environment & Development

摘　　要：自然界中地下水的运动是非常复杂且多变的,用来描述地下水运动的方法有很多种,每一种都有其优势也有其局限性。本文将研究地下水运动的主要方法概括为数学模型法和物理模型法,相同的是,两种方法均是将现实中复杂的水文地质条件概化为简单的水文地质模型,不同的是,数学模型法是通过求解数学模型来研究地下水的运动规律,而物理模型法则是利用相似的物理模型来比拟水文地质模型。The movement of groundwater in nature is very complex and variable.There are many ways to describe groundwater movement.Each has its own advantages and limitations.In this paper,the main methods of studying groundwater movement are summarized as mathematical model method and physical model method・Similarly,both methods generalize the complex hydrogeological conditions in reality into simple hydrogeological models.The difference is that the mathematical model method is to study the motion law of groundwater by solving mathematical models.The physical model rule is to use a similar physical model to compare hydrogeological models.

关 键 词：地下水运动 数学模型法 物理模型法 水文地质模型 

分 类 号：X11[环境科学与工程—环境科学]