特大洪水成因的全球和区域层面:物质和水分平衡(地表水和地下水贡献)的预测和估算问题

T. Trifonova, D. Trifonov, D. Bukharov, Sergei Abrakhin, Mileta Arakelian, S. Arakelian
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引用次数: 1

摘要

传统上,暴雨被认为是洪水发生的主要因素。但是,考虑到世界上完全不同地区的灾难性洪水的一些例子,对水平衡的粗略估计导致有必要提出一个正确的替代假设。我们最简单的模型(考虑降水、蒸发和土壤渗透性)清楚地指出,在一些事件中,潜在积累的水团和观测到的水团之间存在显著差异。这一观察结果提出了降水是必要的想法,但它往往不是灾难性洪水出现和水流收支的充分因素。因此,另一种可用的水源,即地下水,不应被忽视。我们考虑这种现象的原因和条件。在本章中,我们将只集中讨论岩体中危险动力现象的成因和预测。这里特别感兴趣的是水流通过各种花岗岩块体和岩浆成因的地质岩石使用非线性动力学方法。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Global and Regional Aspects for Genesis of Catastrophic Floods: The Problems of Forecasting and Estimation for Mass and Water Balance (Surface Water and Groundwater Contribution)
Traditionally torrential rains are considered to be the main factor of flood emergence. But with some examples of disastrous floods in absolutely different parts of the world, the rough estimation of the water balance results in the necessity to suggest a correct alternative hypothesis. Our simplest model (taking into account precipitation, evaporation, and soil permeability) clearly points out the significant discrepancy in several events between potentially accumulated and observed water masses. This observation puts forward the idea that precipitation is necessary, but it is not often a sufficient factor for disastrous flood emergence and for the water flow budget. Thus, another available water source, i.e., groundwater, should not be ignored. We consider the reasons and conditions for such phenomena. In this chapter, we will focus only on the causes and forecast of dangerous dynamic phenomena in rock masses. Of particular interest here are water flows through various granite massifs and geological rocks of magmatic origin using nonlinear dynamics approaches.
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