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GSPAC water movement in extremely dry area 被引量:4
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作者 HongShou Ll WanFu WANG +2 位作者 GuoBin zhang zhengmo zhang XiaoWei WANG 《Journal of Arid Land》 SCIE 2011年第2期141-149,共9页
Under an extremely arid condition,a PVC greenhouse was built on the top of Mogao Grottoes in gobi area.The results of 235-day constant extraction of condensed water on the greenhouse film and soil water content showed... Under an extremely arid condition,a PVC greenhouse was built on the top of Mogao Grottoes in gobi area.The results of 235-day constant extraction of condensed water on the greenhouse film and soil water content showed that 2.1 g/(m2·d) groundwater moved up and exported into the soil,and a phreatic water evaporation existed in the extreme dry area where the groundwater is buried deeper than 200 m.After a prolonged export,the soil water content in the greenhouse was not lower but obviously higher than the original control ones.According to the monitored parameters including relative humidity and absolute humidity of soil,and temperature outside and inside the greenhouse,it was found that there is the available condition and mechanism for the upward movement of groundwater,and also it can be sure that the exported water was not from the soil and atmosphere outside the greenhouse.Phreatic water,an important source for soil water,interacts with atmosphere moisture via soil respiration.Soil salinity also has important effects on soil water movement and spatial-temporal heterogeneity.The extremely dry climate,terrestrial heat and change of upper soil temperature are the fundamental driving forces of water transportation and phreatic water evaporation in the Groundwater-Soil-Plant-Atmosphere Continuum(GSPAC) system. 展开更多
关键词 greenhouse method GSPAC system extremely dry area water movement
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The Influence of Two Natural Reinforcement Fibers on the Hygrothermal Properties of Earthen Plasters in Mogao Grottoes of China
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作者 Wenbei Bi Zengfeng Yan +3 位作者 Huan Zhao Lixin Sun Xudong Wang zhengmo zhang 《Journal of Renewable Materials》 SCIE EI 2020年第12期1691-1710,共20页
Murals in Mogao Grottoes consist of three parts:support layer,earthen plasters and paint layer.The earthen plasters play a key role in the preservation of murals.It is a mixture of Dengban soil,sand,and plant fiber.Tw... Murals in Mogao Grottoes consist of three parts:support layer,earthen plasters and paint layer.The earthen plasters play a key role in the preservation of murals.It is a mixture of Dengban soil,sand,and plant fiber.Two different natural fibers,hemp fiber and cotton fiber,were reinforced to earthen plasters in the same percentage to evaluate the influence on hygrothermal performance.The two types of earthen plasters were studied:one containing hemp fiber in the fine plaster(HFP)and the other containing cotton fiber in the fine plaster(CFP).Specific heat capacity,dry thermal conductivity,water vapor permeability,and sorption isotherms were investigated.The results showed that the difference between two natural fibers has much more impact on the hygric properties(water vapor permeability and sorption isotherms)of earthen plasters than on their thermal performance(specific heat capacity and dry thermal conductivity).The CFP with higher density has higher thermal conductivity than the HFP with lower density.But no significant differences of specific heat capacity were observed.Compared with HFP,CFP used in murals can reduce the rate of water transfer and prevent salt from transferring water to the mural surface.The overall findings highlight that all these features of CFP are beneficial to the long-term preservation of murals.The study of the earthen plasters in Mogao Grottoes is of general significance,and the measured properties can be used to obtain coupled heat and moisture analysis of the earthen plasters and to dissect the degradation mechanism of murals. 展开更多
关键词 Earthen plasters natural reinforced fibers hygrothermal properties dry thermal conductivity water vapor permeability sorption isotherms
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莫高窟PM_(10)浓度与气象要素的关系 被引量:1
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作者 杨小菊 赵学勇 +5 位作者 武发思 张正模 薛平 陈章 汪万福 张国彬 《中国沙漠》 CSCD 北大核心 2021年第6期54-64,共11页
采用2018年敦煌莫高窟第16窟窟内与窟区PM_(10)浓度及气象数据,分析PM_(10)时空分布特征及其影响因素。结果表明:(1)两处监测点PM_(10)浓度主要分布在50μg·m^(-3)以下,受重污染天气影响较小;春、冬、秋、夏季依次降低,窟区PM_(10... 采用2018年敦煌莫高窟第16窟窟内与窟区PM_(10)浓度及气象数据,分析PM_(10)时空分布特征及其影响因素。结果表明:(1)两处监测点PM_(10)浓度主要分布在50μg·m^(-3)以下,受重污染天气影响较小;春、冬、秋、夏季依次降低,窟区PM_(10)浓度在春、冬季高于窟内,夏、秋季反之。(2)PM_(10)浓度3月最高,9月最低,5—9月窟内月均值高于窟区。PM_(10)污染日数窟内5月最多,而窟区3、5月较多。(3)PM_(10)浓度日变化曲线在春季和秋季呈“双峰”型,夏季和冬季呈“单峰”型。(4)在半封闭环境的洞窟内,沙尘暴发生前后,PM_(10)浓度达到极值及恢复至原来水平的时间均滞后于窟区。(5)在不同季节PM_(10)浓度与气温、风速和降水呈负相关。除秋季外,PM_(10)浓度与相对湿度、气压呈正相关。(6)窟区全年主风向为ESE,在冬春两季,此风向PM_(10)浓度最高,PM_(10)主要来自三危山前的戈壁滩、干涸的大泉河河道以及窟前裸露的地表积尘。 展开更多
关键词 莫高窟 PM 变化特征 气象要素 文化遗产保护
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