• ISSN 2305-7068
  • Indexed by ESCI CABI CSA
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2013 Vol. 1, No. 1

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Application of the “Accurate Control Groundwater Resources” Theory in Containment of Groundwater Resource Exhaustion Trend
Jiansheng Shi, Hongtao Liu, Zhiyuan Liu, Tieliu Chen
2013, 1(1): 1-10.
Abstract(483) PDF(1121)
The continued sustainable economic development of china depends in part, to the scientific management of China’s precious groundwater resources in the coming years. Groundwater resource scarcity is a common underlying problem across China, in addition, the large-scale groundwater exploitation for human consumption over recent decades has resulted in a series of environmental geological problems. As a result of these problems, the national economics in china have been seriously affected. In order to prevent groundwater resource exhaustion and environmental geology deterioration, “accurate control of groundwater resources (ACGR)” theory and its support system were established in this article, and the related prevention measures of the ACGR theory, such as accurate irrigation, accurate supply water, and accurate subsidies, were proposed. This paper highlights the ACGR theory as an efficient and essential way to achieve the sustainable groundwater resource management, which can be applied to countries such as China.
Groundwater Use in the Selenge River Basin, Mongolia
B.T. Hiller, N. Jadamba
2013, 1(1): 11-32.
Abstract(845) PDF(1472)
The Selenge River Basin occupies a total area of 447,000 km2, of which 343,000 km2 is located within Mongolia (the remainder is in Russia). The basin is characterized by an extreme continental climate, consisting of harsh, cold, dry winters and short, hot summers. Annual average temperatures are approximately -4°C and annual rainfall ranges from 220 mm to 450 mm.The Selenge River Basin is a critical groundwater resource for Mongolia. Greater than 55% (~1.5 million) of Mongolia’s population resides within the basin and, during 2003, an estimated average of 700,000 m3/day of water was abstracted from the basin’s groundwater system. The basin services Mongolia’s largest cities and industries (including the rapidly expanding mining sector) as well as important traditional pastoral ranges.
A Study on Infiltration and Groundwater Development in the Influent Zone of the Perched Lower Yellow River
Jingli Shao, Yali Cui, Yunzhang Zhao
2013, 1(1): 46-53.
Abstract(584) PDF(1074)
A three-dimension flow model based on the hydrogeological conditions within the influent zone of the Yellow River in Henan Province, Yuanyang, China, was set up using FEFLOW. The interaction of the Yellow River and the groundwater was simulated under various pumping scenarios. For the planned water supply area, simulation results indicate that, within 10 years’ pumping at a rate of 4.86′108m3/a, the shallow groundwater flow and infiltration from Yellow River will be stabilized . After 10 years pumping, the infiltration will increase to 3.22′108m3/a ?and take approximately 70% of the pumping water.
Groundwater quality Management in China
Aizhong Ding, Lirong Cheng, Steve Thornton, Wei Huang, David Lerner
2013, 1(1): 54-59.
Abstract(500) PDF(976)
Groundwater quality is of vital importance in groundwater safety especially for the purpose of water supply, its management becomes more and more necessary as groundwater contamination has threaten its safe use in China. The article analyzed the contamination sources of groundwater and impact of contamination on human health and water supply, the knowledge gaps were pointed and recommendations were made for groundwater quality management in China.
Comparison of Three Brine Migration Models in Groudwater
Yu Liu
2013, 1(1): 70-73.
Abstract(489) PDF(1193)
Three brine migration models in underground waters were compared to solve the problem of high-density brine migration in underground fresh waters. As shown by the example of brine occurrence in salt dumps, it is preferable to use the model of variable-density solution migration for real layered hydrogeological systems.
Organic Contamination of Soil and Goundwater in the Piedimont Plain of the Taihang Mountains
Zhao Wang, Jiansheng Shi, Zhaoji Zhang, Yuhong Fei
2013, 1(1): 74-81.
Abstract(690) PDF(1347)
The risk of groundwater contamination following the infiltration of waste surface water, is of great interest, particularly in areas experiencing water shortage. In this study, the distribution characteristics of contaminants along the Cihe River, in the piedimont plain of the Taihang Mountains, China, was investigated by measuring the soil and water samples. The main organic contaminants detected in different media include hydrocarbons, chlorinated hydrocarbons, polycyclic aromatic hydrocarbons, and pesticides. The main contaminants found in different media are mostly derived from the river water, which can be seen from the results of waste water from the river and groundwater, from the soil samples from different depth and distance of the profiles along the river. The distribution characteristics showed that there has been a natural attenuation of the contaminants from the river during their transportation through the soils and groundwater. The sorption of organic compounds to soil organic matter is thought to be a main mechanism of natural attenuation.
Stable Isotope Composition of Rainfall, Surface Water and Groundwater along the Yellow River
Yan Zhang, Shuai Song, Jing Li, Fadong Li, Guangshuai Zhao, Qiang Liu
2013, 1(1): 82-88.
Abstract(694) PDF(1196)
The intention of this work is to consider the stable isotopic compositions of oxygen and deuterium in rainfall, surface water and groundwater along the Yellow River in the North China Plain (NCP). This demonstrated that the δ18O values in groundwater varied from –10.17 to –6.85‰, with mean value of –8.76‰, and that the δD ranged from –68.7 to –58.0‰, with mean value of –63.4‰, respectively. The δ18O values in surface water varied from –8.36 to 1.32‰, with mean value of –6.8‰, and δD ranged from –64.4 to –35.1‰, with mean value of –57.6‰, respectively. Further, The range of Cl- values of groundwater varied from 5.9 to 340.5 mg/L and that values ranged from 30.1 to 81.9 mg/L in surface water samples and Na+ value changed from 27.4 to 321 mg/L in groundwater, while that in surface water varied from 24.8 to 50.5 mg/L. Most of the points fall below the GMWL?, but are close to the LMWL.? Therefore the results indicated that the groundwaters along the Yellow River were influenced by rainfall in heavy events and surface water.
Study on Ecological Environment and Sustainable Land Use Based on Satellite Remote Sensing
Jiankang Zhang, Yanpei Cheng, Hua Dong, Qingshi Guo, Kun Liu, Fawang Zhang
2013, 1(1): 89-96.
Abstract(493) PDF(1218)
GIS and RS techniques have been applied to interpret satellite data in 1992, 2000 and 2010. Further, the ecological environment factors of these three periods and the data for various types of land use have been obtained. LUDI in the Amur River Basin from 1992 to 2010 has been quantitatively analyzed by using the land use dynamic (LUDI) model and of land use transfer matrix model. The results indicated that from 1992 to 2010 the LUDI of land desertification is greatest, and is the most dramatic change. The comprehensive land use dynamic in the study area is 15.25, hence the land type is characterized by rapid change. In addition the area of woodland and farmland continues to increase, which has been mainly transformed from the mixture of forestland and grassland, marsh and wetland, this is an outcome of the production of shelter-forest plantation in North China, Northeast China and Northwest China. In the ten years period of the study, the area of desertified land has increased, changing mainly from a mixture of woodland and grassland. This study can rovide data for eco-geological environment management.
Source and Formation of the Arsenic in Ground Water in Hanoi , Vietnam
Do Van Binh
2013, 1(1): 102-108.
Abstract(477) PDF(928)
The problem of Arsenic source in groundwater has yet been addressed thoroughly. From the results of the analysis of samples, this article gives the statement that the Arsenic in groundwater of Quaternary sediments in Hanoi has mainly natural source, with the impact of man-made factors (industrial waste water, use of crop protection products, etc.). The article also explains the formation of Arsenic in groundwater in Hanoi area is closely related to the reduction by two main mechanisms, reducing mechanism of oxyhydroxit (Fe3 + OHAs) As liberation by microorganisms and reducing mechanism of As adsorbed on iron oxide or oxyhydroxit replaced by bicarbonate. The process of oxidation of minerals containing As is needed to be researched more.