【摘 要】
：
吸湿凝结水作为干旱半干旱地区除降雨外主要的水分来源,具有十分重要的生态水文学意义。以青海共和盆地高寒沙区1997年植被恢复区生物土壤结皮吸湿凝结水为研究对象,2018年5—9月采用自制微渗仪观测吸湿凝结水量,同时观测近地层空气温湿度和土壤温湿度。结果表明:观测期间,不同类型结皮吸湿凝结水量存在差异,表现为苔藓结皮>藻类结皮>物理结皮>流沙,且差异性与观测时间无关;吸湿凝结水量与近地层空气湿度正相关
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吸湿凝结水作为干旱半干旱地区除降雨外主要的水分来源,具有十分重要的生态水文学意义。以青海共和盆地高寒沙区1997年植被恢复区生物土壤结皮吸湿凝结水为研究对象,2018年5—9月采用自制微渗仪观测吸湿凝结水量,同时观测近地层空气温湿度和土壤温湿度。结果表明:观测期间,不同类型结皮吸湿凝结水量存在差异,表现为苔藓结皮>藻类结皮>物理结皮>流沙,且差异性与观测时间无关;吸湿凝结水量与近地层空气湿度正相关,与近地层空气温度、土壤温度湿度负相关,且相关性与地表类型无关;吸湿水凝结过程主要受近地层空气温湿度的影
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