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The groundwater divide between western and eastern coastlines moved during different reclamation stages.
Lake Hampen, (Central Jutland, Denmark) is located high in the landscape near a seasonal moving groundwater divide.
The location of hillslope hydrologic boundaries, including the groundwater divide and no-flow boundary underlying the hillslope, changed the transit time distribution less markedly.
The groundwater transfer times between the groundwater divide line and the wells are calculated thanks to flow and transport modelling, used in a backward particle tracking mode.
An analytical solution is presented for delineating the catchment zone of a well located near a groundwater divide in a recharged aquifer.
In case of an injection well, the catchment zone comprises the whole aquifer when the well is sufficiently close to the groundwater divide, and otherwise consist of an infinite but laterally bounded zone in the direction away from the groundwater divide.
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Any variation in the precipitation, along with variations in atmospheric temperature, not only affects input (recharge) and output (discharge) components of a groundwater system, but influence its' water quality (Sukhija et al. 1998), modify the groundwater flow network, groundwater divides may move position (Dragoni and Sukhija 2008).
On the basis of chemical analysis groundwater is divided into three distinct fields two triangular fields and one diamond-shaped field.
Thirty-two groundwater samples were divided into four types of groundwater (I, pyrite-oxidation; II, iron- and sulfate-reducing; III, sulfate-reducing; and IV, anthropogenic and others).
Subsequently, the groundwater yield was divided into high (⩾11 m3/h) and low yields (<11 m3/h) respectively, based on the groundwater classification standard recommended by Department of Mineral and Geosciences (JMG), Malaysia.
According to permeability indices, the groundwater may be divided into class I, II and III.
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