PDF HTML阅读 XML下载 导出引用 引用提醒 应用拱棚-空调法对极干旱区降水的模拟回收 DOI: 10.5846/stxb201301290185 作者: 作者单位: 敦煌研究院保护所,古代壁画保护国家文物局重点科研基地;敦煌研究院保护所,古代壁画保护国家文物局重点科研基地;敦煌研究院保护所;敦煌研究院保护所;敦煌研究院保护所,古代壁画保护国家文物局重点科研基地;敦煌研究院保护所 作者简介: 通讯作者: 中图分类号: 基金项目: 国家自然基金项目(41363009, 31070344, 31260136); 国家科技支撑项目(2013BAC07B02); 甘肃省科技计划项目(1308RJZF290); 敦煌研究院院级课题(201306) Application of a greenhouse air-conditioning method to simulate take-back of rainfall in an extremely arid area Author: Affiliation: The Conservation Institute of Dunhuang Academy,,, Fund Project: 摘要 | 图/表 | 访问统计 | 参考文献 | 相似文献 | 引证文献 | 资源附件 | 文章评论 摘要:拱棚法监测表明极干旱区存在潜水蒸发,而土壤温湿度监测表明,土壤水分具备向下运转的条件,这意味着拱棚所监测的水分可能来自降水,极干旱区并不存在深埋潜水蒸发.因此,研究降水的最终去向非常重要.为此笔者应用拱棚-空调法进行对极干旱区降雨模拟回收.结果表明,在极干旱条件下占该区85%以上频次的5 mm的降水经90 d可完全蒸发和回收.回收过程中,棚内地上50 cm 的相对湿度(RH)和绝对湿度(AH)分别较棚外增高12.10%和3.50 g/m3,这使降水的回收时间大为延长;另外,土壤内部的温湿度监测表明,洒水后30 cm土壤的温度、RH、AH分别高于棚外对照1.46 ℃、4.17%和2.50 g/m3,说明有一定数量的降水通过膜下土壤侧向流向了外部,增加了收集时间.回收实验证明极干旱区降水可完全蒸发,该区存在潜水蒸发与GSPAC(Groundwater-Soil-Plant-Atmosphere Continuum)水分的向上运转. Abstract:A preliminary greenhouse air-conditioning method demonstrates that there is phreatic water evaporation of deeply buried phreatic water in an extremely arid area. Soil-moisture monitoring shows that most daily fluctuation of moisture in the shallow soil layer of 0-60 cm enters deeper layers as water vapor; only 2‰ of this daily fluctuation water enters the atmosphere and evaporates. Monitoring of 0-500 cm soil depths shows that during May through October (the principal rainy season), temperature and absolute humidity in upper soil layers are greater than in lower layers. According to the law of water vapor migration, moisture moves from regions of higher temperature and humidity to those with lower temperature and humidity. Thus, in the aforementioned season within an extremely arid area, conditions may be suitable for rainwater vapor to move downward to the subsoil. This may mean that some rainwater does not evaporate into the atmosphere but penetrates the earth in such areas, and precipitation is likely the main source of deep soil moisture. This suggests there is no phreatic water evaporation of deeply buried phreatic water in extremely arid areas. Based on this hypothesis, a closed greenhouse with air-conditioning system was constructed in the arid area of the Mogao Grottoes in the Gobi Desert. In this greenhouse, we conducted a simulation recycling experiment of 5-mm precipitation via an air-conditioning condensation method. In this way, we first traced where rainwater went. Temperature and humidity were controlled by refrigeration and air-conditioning condensation, which made the temperature and humidity inside the greenhouse approach that of the outside. To understand characteristics of rainfall evaporation in extremely arid areas, the quantity of condensation water was monitored daily. We analyzed temperature and humidity variations, which were monitored by HOBO monitors in the soil, to understand the rainfall infiltration and evaporation process. This confirmed the ultimate flow direction of precipitation, and whether it completely evaporated. This approach was used to determine if there was phreatic water evaporation. The results showed that 5 mm of precipitation, which represented 85% of the frequency of precipitation in this area, completely evaporated. The relative and absolute humidities of the 50 cm above ground within the greenhouse were 12.10% and 3.50 g/m3 greater than outside it, respectively. These results caused the experimental time to be longer than for actual evaporation. In addition, soil temperature and humidity monitoring indicated that after water was sprinkled in the greenhouse, soil temperature, relative humidity and absolute humidity at 30 cm depth were greater by 1.46℃, 4.17% and 2.50 g/m3 than the outside control, respectively. This means that during evaporation, a certain amount of rainfall reached the outside through the greenhouse side soil, under the greenhouse film. This was another reason why the precipitation evaporation collection time was greatly extended. The collection time of 90 days may be much longer than the actual time for natural evaporation, but it confirmed the effectiveness of the rainfall recycling experiment. After complete take-back of all the simulated rainwater, soil moisture did not decline, but increased. The phreatic evaporation speed also increased, which means that precipitation pulsation has a certain control on evaporation of the phreatic water. It was demonstrated that there is phreatic evaporation, and soil water was supplemented by this water. Groundwater-Soil-Plant-Atmosphere Continuum (GSPAC) movement was upward, and the precipitation could completely evaporate. 参考文献 相似文献 引证文献