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Simulation on the Water Transporting Process in Zoige Wetland SPAC System and its Eco-hydrological Effect

机译:Zoige湿地SPAC系统水运过程的仿真及其生态水文效应

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As the largest plateau wetland in the world, Zoige Wetland is suffering from multiple deterioration along with the shrinking of marshland and other water bodies and desertification of grassland. Field tests as well as lab experiments with regard to hydrology observation, soil water monitoring and botanic sampling were conducted in the transition zone of wetland. A SPAC (Soil Plant Atmosphere Continuum) model, verified by data obtained from field tests and lab experiments, was applied for the first time in Zoige Wetland to study the water flow among SPAC system. Result shows that 1) the Zoige Wetland SPAC model could describe the eco-hydrological process appropriately; 2) the ideal groundwater level for Trollius Paluster which is. widely distributed in Zoige Wetland is 60 ~ 100cm underground, whereas 0~60cm and 100~250cm are also adaptable for them.
机译:作为世界上最大的高原湿地,Zoige湿地正在遭受多次恶化,随着沼泽地和其他水域和草原的荒漠化的萎缩。在湿地的过渡区进行了现场测试以及关于水文观察,土壤水监测和植物抽样的实验室实验。通过现场测试和实验室实验获得的数据验证的SPAC(土壤植物气氛连续核)模型是在Zoige湿地中的第一次应用于SPAC系统之间的水流。结果表明,1)Zoige湿地SPAC模型可以适当描述生态水文过程; 2)Trollius Paluster的理想地下水位。广泛分布在Zoige湿地的地下60〜100cm,而0〜60cm和100〜250cm也适用于它们。

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