中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
STUDY OF SOIL WATER MOVEMENT AND GROUNDWATER RECHARGE FOR THE LOESS TABLELAND USING ENVIRONMENTAL TRACERS

文献类型:期刊论文

作者Cheng, L.1,2; Liu, W.1; Li, Z.3; Chen, J.1,4
刊名TRANSACTIONS OF THE ASABE
出版日期2014
卷号57期号:1页码:23-30
关键词Deuterium Land Use Oxygen-18 Piston Flow Preferential Flow
文献子类Article
英文摘要Groundwater is the primary water resource for human use on the Loess Tableland of China; however, the depletion of groundwater has been very severe in recent years. To understand the reasons for groundwater depletion, it is necessary to understand its recharge mechanisms. The objective of this study is to reveal the mechanisms of groundwater recharge on the Loess Tableland using deuterium and oxygen-18 in precipitation, in soil water under three land use types (natural grassland, wheat field, and apple orchard), and in groundwater Results indicate that piston flow and preferential flow coexist in rainfall infiltration; however their occurrences are greatly influenced by land use type. They both occurred in the natural grassland and wheat field; however; only piston flow was detected in the apple orchard. Groundwater is likely to be recharged by both piston flow and preferential flow through the unsaturated zone, while preferential flow should be the main recharge mechanism, as the isotopic composition of the groundwater is very close to that of precipitation while quite different from that of deep soil water However, groundwater recharge by preferential flow only occurred in the natural grassland or wheat field, but not in apple orchard due to its thick dry soil layer. Regarding groundwater recharge by piston flow, it possibly occurs in most years for the natural grassland and in wet years for the wheat field; however, it is possibly difficult for the apple orchard to recharge groundwater by piston flow. The above results suggest that the conversion of farmland to apple orchard can affect the natural mode of the water cycle and reduce groundwater recharge on the Loess Tableland; therefore, attention should be paid to adjustments of land use.
WOS关键词STABLE-ISOTOPES ; DRY SOILS ; UNSATURATED ZONE ; TRITIUM PROFILES ; NORTH CHINA ; O-18 ; DEUTERIUM ; OXYGEN ; EVAPORATION ; HYDROGEN
语种英语
WOS记录号WOS:000333774700003
出版者AMER SOC AGRICULTURAL & BIOLOGICAL ENGINEERS
源URL[http://ir.igsnrr.ac.cn/handle/311030/68449]  
专题中国科学院地理科学与资源研究所
通讯作者Liu, W.
作者单位1.Chinese Acad Sci & Minist Water Resources, State Key Lab Soil Eros & Dryland Fanning Loess P, Inst Soil & Water Conservat, Yangling 712100, Shaanxi, Peoples R China
2.Pingdingshan Univ, Coll Resource & Environm Sci, Pingdingshan, Peoples R China
3.Northwest A&F Univ, Coll Nat Resources & Environm, Yangling, Peoples R China
4.Univ Quebec, Dept Construct Engn, Montreal, PQ, Canada
推荐引用方式
GB/T 7714
Cheng, L.,Liu, W.,Li, Z.,et al. STUDY OF SOIL WATER MOVEMENT AND GROUNDWATER RECHARGE FOR THE LOESS TABLELAND USING ENVIRONMENTAL TRACERS[J]. TRANSACTIONS OF THE ASABE,2014,57(1):23-30.
APA Cheng, L.,Liu, W.,Li, Z.,&Chen, J..(2014).STUDY OF SOIL WATER MOVEMENT AND GROUNDWATER RECHARGE FOR THE LOESS TABLELAND USING ENVIRONMENTAL TRACERS.TRANSACTIONS OF THE ASABE,57(1),23-30.
MLA Cheng, L.,et al."STUDY OF SOIL WATER MOVEMENT AND GROUNDWATER RECHARGE FOR THE LOESS TABLELAND USING ENVIRONMENTAL TRACERS".TRANSACTIONS OF THE ASABE 57.1(2014):23-30.

入库方式: OAI收割

来源:地理科学与资源研究所

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