RESOURCES AND ENVIRONMENT IN THE YANGTZE BASIN >> 2017, Vol. 26 >> Issue (02): 257-263.doi: 10.11870/cjlyzyyhj201702011

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CHARACTERISTICS OF SOIL WATER TRANSPORT IN DIFFERENT AGED PADDY FIELDS

YANG Yan1,2, YI Jun1,2, LIU Mu-xing1,2, ZHANG Jun1,2, LI Sheng-long1,2   

  1. 1. Hubei Province Key Laboratory for Geographical Process Analysis & Simulation, Wuhan 430079, China;
    2. College of Urban and Environmental Sciences. Central China Normal University, Wuhan 430079, China
  • Received:2016-07-14 Revised:2016-10-23 Online:2017-02-20
  • Supported by:
    National Natural Science Foundation of China (41601215, 41001125);Key Program of Natural Science Foundation of Hubei Province (2015CFA141);Central China Normal University Fund (CCNU16A05015, CCNU15A05002)

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Abstract: Based on the field dye tracing experiment and laboratory analysis of soil samples, the characteristics of soil water transport in different aged paddy fields were revealed. This study is expected to provide scientific basis for the reasonable filed water management. The results showed that significant differences of physical and chemical soil properties between new paddy field (NF, aged 17 years) and old paddy field (OF, aged more than 100 years), which was expected to affect the soil water movement processes. Water percolation was more likely to occur in the NF, which was identified by the higher saturated hydraulic conductivity (KS) in the NF (13.98~78.35 cm/d) than that in the OF (4.35~49.37 cm/d). Highest KS was observed in the plow layer, followed by the subsoil layer, and lowest in the plough pan. More obvious vertical percolation was observed in the NF than that in the OF, characterized by the deeper stained depth. For the OF, highest stained area was observed in the plow layer (48.52%), followed by the subsoil layer (3.17%), and lowest in the plough pan (0.20%). Except for the plow layer, NF was characterized by higher stained area and more obvious preferential flow paths in other soil layers than the OF. Stronger lateral water flow was observed in the OF (15.35%) than that in the NF (8.45%), which was characterized by the more stained area in the OF than the NF, and mainly distributed in the plow layer. In order to reduce the water losses in the paddy field, more attention should focus on the lateral water lose in the inner field-bund-canal transition zone for the OF, and the irrigation strategies of more times with less single irrigation amount was suitable for the NF.

Key words: paddy field, dye tracing, vertical percolation, lateral flow, preferential flow, Jianghan Plain

CLC Number: 

  • S152.5
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