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浙江瑶琳洞风化碳酸钙景观复生试验中CO_2吸收动力学研究
杨京蓉1; 林钧枢1; 王来洪2; 宋林华1
1999
Source Publication中国岩溶
ISSN1001-4810
Volume018Issue:004Pages:13
Abstract在H2O-CO2-CaCO3的系统中,因喀斯特水中逸出O2,导致CaCO3沉积,形成千姿百态,琳琅满目的洞积物,如石笋,钟乳石,石林,石葡萄,卷曲石等等。由于洞穴环境的变化,使洞穴沉积石产生严重的风化作用。然而,我们试用钙碱性溶液吸收CO2,产生CaCO3沉积,可使风化的洞穴碳酸钙景观恢复其美学价值。
Language英语
Document Type期刊论文
Identifierhttp://ir.igsnrr.ac.cn/handle/311030/116486
Collection中国科学院地理科学与资源研究所
Affiliation1.中国科学院地理科学与资源研究所
2.浙江瑶琳洞风景旅游管理处
First Author Affilication中国科学院地理科学与资源研究所
Recommended Citation
GB/T 7714
杨京蓉,林钧枢,王来洪,等. 浙江瑶琳洞风化碳酸钙景观复生试验中CO_2吸收动力学研究[J]. 中国岩溶,1999,018(004):13.
APA 杨京蓉,林钧枢,王来洪,&宋林华.(1999).浙江瑶琳洞风化碳酸钙景观复生试验中CO_2吸收动力学研究.中国岩溶,018(004),13.
MLA 杨京蓉,et al."浙江瑶琳洞风化碳酸钙景观复生试验中CO_2吸收动力学研究".中国岩溶 018.004(1999):13.
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