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Salt Hazard of Earthen Monuments Induced by Capillary Rise

机译:毛细血管上升引起的土方遗迹的盐害

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摘要

Re-distribution and re-crystallization of the soluble salts by capillary water migration in ancient earthen structures results in salt efflorescence which is characterized by granular disaggregation and crumbling.Laboratory capillary water rise tests were conducted on compacted silt soil from ancient Jiaohe Ruins in Xinjiang,China to clarify the responsibility of salts in damage of earthen monuments.Distribution of water contents,pH,electric conductivity and soluble salts of soil liquid after capillary tests illustrated that NaCl accumulation is predominant at the capillary fringe while Na2SO4 at the other capillary front area.Within the capillary rise area along the water migration direction,less soluble,moderately soluble and most soluble salts tend to crystallize out and result in salt crest,salt efflorescence and dark appearance in correspondence.
机译:古代土结构中毛细水迁移导致可溶性盐的重新分布和重结晶导致盐的风化,其特征是颗粒的分解和破碎。对新疆古代交河遗址的压实粉砂土进行了实验室毛细水上升试验,中国明确了盐对土石碑破坏的责任。毛细管试验后水含量,pH,电导率和土壤液体可溶性盐的分布表明,NaCl积累主要发生在毛细管边缘,而Na2SO4则存在于其他毛细管前沿。在沿水运移方向的毛细上升区域内,难溶,中溶和最易溶的盐倾向于结晶出并相应地导致盐峰,盐风化和深色外观。

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