RESEARCH ON ORIGIN AND CURRENT STATUS OF SEA (SALT ) WATER INTRUSION IN COASTAL ZONE OF QINGDAO

XIAO Fei; ZHOU Yonghua; CHEN Xiaoying

2012 Vol. 28, No. 5

Article Contents

Article navigation > Marine Geology Frontiers > 2012 > 28(5): 54-58

Next Article Previous Article

XIAO Fei, ZHOU Yonghua, CHEN Xiaoying. RESEARCH ON ORIGIN AND CURRENT STATUS OF SEA (SALT ) WATER INTRUSION IN COASTAL ZONE OF QINGDAO[J]. Marine Geology Frontiers, 2012, 28(5): 54-58.

Citation:

XIAO Fei, ZHOU Yonghua, CHEN Xiaoying. RESEARCH ON ORIGIN AND CURRENT STATUS OF SEA (SALT ) WATER INTRUSION IN COASTAL ZONE OF QINGDAO[J]. Marine Geology Frontiers, 2012, 28(5): 54-58.

RESEARCH ON ORIGIN AND CURRENT STATUS OF SEA (SALT ) WATER INTRUSION IN COASTAL ZONE OF QINGDAO

1 Key Laboratory of Renewable Energy and Gas Hydrate, Guangzhou Institute of Energy Conversion, Chinese Academy of Sciences, Guangzhou 510640, China;
2 Guangzhou Center for Gas Hydrate Research, Chinese Academy of Sciences, Guangzhou 510640, China;
3 Graduate School of the Chinese Academy of Sciences, Beijing 10049, China

Received Date: 04 January 2012

Abstract

Abstract

Sea (salt ) water intrusion is one of main geologic hazards in coastal Qingdao. It mostly occurs around main estuaries into the Jiaozhou Bay. Sea water and ancient seawater or high mineralized underground salt water intrude to the land along the aquifer due to over exploitation of groundwater around the intrusion zones. As the result, groundwater resources are contaminated. Based on the study of the formation mechanism of the disaster, prevention measures are proposed in this paper.
- sea (salt) water intrusion /
- underground water /
- coastal area