Wang Yanrong, Zeng Yanjun, Zhang Baoling, Ta Lateng
College of Pastoral Agriculture Science and Technology, Lanzhou University, Gansu Grassland Ecological Research Institute, Lanzhou.
Ying Yong Sheng Tai Xue Bao. 2002 Aug;13(8):962-6.
Water distribution pattern and water use-efficiency in soil-plant-atmosphere system for light, medium, and heavy degraded Reaumuria soongorica grasslands were studied in Alashan region of Inner Mongolia. The total precipitation in 2001 was 124.3 mm, of which 119.4 mm occured during experimental period. Soil water content (SWC) in 10-40 cm layer was greatly affected by the evapotranspiration. The SWC in 10-20 cm layer of medium degraded grassland paddock was significantly lower (P < 0.05), and the SWC in 20-40 cm layer of light degraded paddock was lower than that of other paddocks due to different transpiration rate and root distribution depth between the main co-existing plant species of R. soongorica and Cleistogenes soongorica in the paddocks. The annual average bare land evaporation and R. soongorica population transpiration were 30.6 mm and 11.9 mm, respectively. As the grassland further degraded, the bare land evaporation and transpiration through Peganum nigellastrum population, a degradation indicating plant species, increased, while the transpiration of R. soongorica decreased. In addition, the water use-efficiency of the grassland and dominant plant species markedly decreased with the increasing grassland degradation. Compared to the light degraded paddocks, for instance, the water use-efficiency of medium and heavy degraded paddocks were reduced by 14.6% and 46.1% for total biomass production, and by 37.8% and 73.8% for R. soongorica, respectively.
以内蒙古阿拉善地区轻度、中度和重度退化的红砂草原为研究对象,对土壤-植物-大气系统中的水分分布格局和水分利用效率进行了研究。2001年的总降水量为124.3毫米,其中119.4毫米出现在实验期内。10-40厘米土层的土壤含水量受蒸散作用影响较大。中度退化草地围场10-20厘米土层的土壤含水量显著较低(P<0.05),轻度退化围场20-40厘米土层的土壤含水量低于其他围场,这是由于围场中红砂和糙隐子草这两种主要共存植物物种的蒸腾速率和根系分布深度不同所致。年平均裸地蒸发量和红砂种群蒸腾量分别为30.6毫米和11.9毫米。随着草地进一步退化,作为退化指示植物物种的骆驼蓬种群的裸地蒸发量和蒸腾量增加,而红砂的蒸腾量减少。此外,随着草地退化程度的增加,草地及其优势植物物种的水分利用效率显著降低。例如,与轻度退化围场相比,中度和重度退化围场总生物量生产的水分利用效率分别降低了14.6%和46.1%,红砂的水分利用效率分别降低了37.8%和73.8%。