中国三北地区冻结滞水资源对生态环境建设的效应研究

Study on effects of frozen stagnant water on eco-environmental construction in Three-North Area of China

  • 摘要: 依据野外观测和室内模拟实验研究资料分析冻结滞水对西北地区生态环境建设的效应,冻结滞水是指冬季冻结作用在包气带冻土层内形成的固态地下水,具有形成机制独特、富水性倒置和独立的水盐动态特征,对生态环境建设产生双重效应。冻结滞水量比冻结前土壤含水量一般增加8%~25%,最高可达39.51%,冻胀区可达300%。在三北地区冻结滞水是天然和人工树木等植被越冬、春季繁衍期间水分代谢均衡的主要水资源,甚至是唯一水资源,是三北地区生态环境建设成败的主导因素之一。当冻结滞水量平均<5%时,天然林和人工林等植被衰亡,可加速荒漠化,当冻结滞水量达过饱和状态时,则易形成沼泽化、盐渍化等不良地质现象,导致生态环境恶化。控制冻结滞水量对西北地区建设林业工程、优化生态环境和可持续发展至关重要。

     

    Abstract: Based on the field observation and simulation in laboratory,the effects of frozen stagnant water (FSW) on ecoenvironmental construction of Northwest area were analyzed. FSW is seasonal solid underground water, formed by freezing effects in winter in the frozen soil layer of independent water and salt dynamics.It has positive and negative effects on ecoenvironmental construction. FSW generally increases the amount of water by 8%~25%.The maximum water content is 39.51%.The water content is 300% at frozen lumps on the ground. It is indispensable or even the unique water source for natural forest and manual vegetation lived through the winter, vegetation growth in spring, water metabolism, and also is a central factor of ecological balance in Three-North area. When the FSW content <5%,it brings about contabescence for natural forest and manual vegelation, and acceleration of desertification but when water content arrives at immoderate sturated state, some geological phenomena as frozen lumps on the ground, landslides, dents and salingation of swamplifotion are formed, thus accelerating the deterioralion and imbalance of ecology. The control of FSW content is very important to building the engineering of sustainable developing forestry and improving ecoenvironment in Northwest area.

     

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