[an error occurred while processing this directive] ������� 2009, 28(1) 75-81 DOI:     ISSN: 1004-5589 CN: 22-1111/P

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Article by Han, J. 1
Article by 2
Article by Liu, Z. H. 2
Article by 3
Article by Li, Q. 2
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1. �˹�ҵ���������о�Ժ, ���� 100029; 2. ������Դ�����ܵ����о���, ���ܶ���ѧ�ص�ʵ����, ���� ���� 541004; 3. �й���ѧԺ����ѧ�о���, ��������ѧ�����ص�ʵ����, ���� 550002
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���ö�����Զ���¼�ǶԹ���Ū��������Ȫ�޽���ʱ��ˮ��ѧ��̬�仯������, ˮ��CO2 ��ѹ���¶ȺͰ�������ˮ״��������Ȫˮˮ��ѧ��̬�仯����Ҫ���ء����±仯�����꼰̫���������ҹ����, Ӱ����ֲ���������ǿ����ʪ��Ȫˮ����ʴǿ�����Դ��ڸɼ�, ����Ϊ����ʯ����ָ�� ( SIC ) �Ͱ���ʯ����ָ��( SID ) �ϸߡ���ʪ���޽�������������, �¶ȶ�ֲ������Ҫ�������á�

�ؼ����� ������Ȫ   ˮ��ѧ��̬   ֲ��   CO2��ѹ   �¶�   ����   Ū��  
Hydrochemical variation explanation to Landiantang spring in Nongla of Guangxi
HAN Jun1,2, LIU Zai-Hua2,3, LI Qiang2
1. Beijing Research Institute of Uranium Geology, Beijing 100029, China; 2. Key Laboratory of Karst Dynamic, Research Institute of Karst Geology, MLR, Guilin 541004, Guangxi, China; 3. State Key Laboratory of Environmental Geochemistry, Research Institute of Geochemistry, CAS, Guiyang 550002, China
Abstract:

Through the research on Landiantang spring in Guangxi, the authors monitored and analyzed hydro-chemical variations during non-rainfall term, and suggested that the carbon dioxide partial pressure in spring water, temperature and aquifer condition play the key roles in controlling daily geochemical variation of epi-karst spring water. Moreover, insolation strength, rainfall amount and solar radiation affected the vegetation activity. More erosion effectiveness occurred in wetmonths presented by the high value of SIC and SID than in dry season. The temperature controlled the vegetation productivity both in dry and wet seasonswithout precipitation.

Keywords: Landiantang spring   hydro-chemical variation   vegetation activity   carbon dioxide partial pressure   temperature   Nongla   Guangxi  
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