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1)  geochemical variation
表层岩溶系统
1.
Taking six typical epikarst systems in China as examples, the authors summarize their features of geochemical variations, and analyze their environmental significance.
以中国6个典型表层岩溶系统为例,总结了它们的地球化学动态特征,并对其所反映出的环境意义作了分析。
2)  Epikarst water systems
表层岩溶水系统
3)  epi-karst dynamic system
表层岩溶动力系统
1.
It has been found that epi-karst dynamic system is related closely with CO2 content in soil and that temperature and rainfall dominate the seasonal change of CO2 content in soil.
峰丛洼地表层岩溶动力系统与土壤CO2密切相关,土壤CO2体积分数以及表层岩溶带土壤CO2溶蚀量的变化受气温和降雨影响。
4)  epikarst ecosystem
表层带岩溶生态系统
1.
Karst ecosystem is a ecosystem controlled by karst environment, and epikarst ecosystem is the most active part of material exchange and energy flow in karst ecosystem, it is sensitive to the global carbon cycle in Quaternary, especially in late Holocene.
岩溶生态系统是受岩溶环境制约的生念系统,而表层带岩溶生态系统则是岩溶生态系统物质交换和能量流动最活跃的一部分,对全球第四纪尤其是全新世晚期碳循环表现出灵敏的响应。
5)  multilayer karst system
多层岩溶系统
6)  karst system
岩溶系统
1.
Carbonate rocks are widespread along the south Tianshan, where the function of karst system depends on the texture of karst medium.
南天山广泛出露碳酸盐岩地层,其岩溶系统功能取决于岩溶介质结构。
补充资料:L2工业纯铝360℃热轧板表层纵向组织


L2工业纯铝360℃热轧板表层纵向组织


  L2工业纯铝360。0热轧板表层纵向组织
  
说明:补充资料仅用于学习参考,请勿用于其它任何用途。
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