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一、前言运用系统分析方法,是当前研究地F水的一个主要方向。地下水系统的研究,必须综合考虑各种有关因素,诸如能量转化关系、水质与水量之间的演变关系、地下水系统与地表水输入系统和输出系统之间的关系以及地下水动力学与水化学、热力学系统之间的互相关系等,才能得出比较可信的结果。地下水系统分析研究的理论和实践揭示了地下水中多种离子在阳阳、阴阴、阳阴之间或其相应组合及其比率之间存在着彼此制约的复相关关系。在成因上有机地把各种离子之间的比率关系及其分异动态变化进行系统研究,将有助于地震前兆信息的提取和判别,而地下水D函数系列变化特征是提取地震前兆信息的一个值得探讨的新途径和新方法。
I. INTRODUCTION The use of systematic methods of analysis is one of the main directions of the current study of F water. Groundwater system research must take into account various relevant factors such as energy conversion relationships, the evolutionary relationship between water quality and water volume, the relationship between groundwater systems and surface water input and output systems, as well as groundwater dynamics and hydration, thermodynamics System interrelationships, etc., in order to come to more credible results. The theory and practice of groundwater system analysis and research reveal that the multiple ions in groundwater have a complex relationship between Yang Yang, Yin Yin, Yang Yin, or their corresponding combinations and their ratios. It is helpful to systematically study the ratio relationship of various ions and their dynamic changes organically, which will be helpful for the extraction and discrimination of earthquake precursors information. However, the feature series of groundwater D functions is one of extracting the precursory information of earthquakes Worth to explore new ways and new methods.