title: [Relationship between groundwater level in riparian wetlands and water level in the river].
abstract: The development and degradation processes of riparian wetlands are significantly affected by river hydrological processes. By observing the variation of groundwater levels in riparian wetlands at the Kouma section of the Yellow River Wetland, especially that during the period of regulation for water and sediment at the Xiaolangdi Reservoir, relationship between groundwater level in riparian wetlands and flood water level in the river is studied. The results show that groundwater level in riparian wetlands is significantly affected by water level in the river investigated. There is a negative exponential relationship between groundwater level and the distance between wells and river. The correlation coefficient shows the maximum (R2 > 0.98) during the period of regulation for water and sediment. Affected by the cultivation system in the flooding area, distance between monitoring wells and river bank, water level in the river variation of groundwater level in the wetland changed greatly. In artificial wetland, which is far from the river, the inter-annual variation in groundwater levels show a " (see symbol)" shape, while in the farmland, which is close to the river, the inter-annual variation of groundwater levels show a big peak. The groundwater level 400 m from the river is affected by flood events obviously, that in the area which is less than 200 m from the river is significantly affected by flood events in the area which is especially less than that in the area that is less than 100 m from the river, the groundwater level is affected by flood events intensively. The result indicated that there was a very close relationship between groundwater and surface water, and it was the hydrological ecotone between groundwater of riparian wetlands and the river. It is very important that rational protection for this region (very important for the area which is less than 100 m from the river, important for the area that is between 100 m and 200 m from the river) is critical for the conservation of water quality in the river and groundwater quality.
authors.affiliation: Key Laboratory of Water and Sediment Sciences, Ministry of Education, College of Water Sciences, Beijing Normal University, Beijing 100875, China. xuhuashan@hpu.edu.cn
authors.forename: Hua-Shan
authors.initials: HS
authors.lastname: Xu
authors.forename: Tong-Qian
authors.initials: TQ
authors.lastname: Zhao
authors.forename: Hong-Qi
authors.initials: HQ
authors.lastname: Meng
authors.forename: Zong-Xue
authors.initials: ZX
authors.lastname: Xu
authors.forename: Chao-Hong
authors.initials: CH
authors.lastname: Ma
mesh_terms: D002681:China; D055868:Floods; D005618:Fresh Water / Q000032:analysis* / Q000737:chemistry; D045483:Rivers; D014872:Water Movements; D014876:Water Pollution / Q000517:prevention & control; D014881:Water Supply / Q000032:analysis*; D053833:Wetlands