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| Type: | Resource | |
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| Created: | Feb 08, 2023 at 3:33 p.m. | |
| Last updated: | Feb 08, 2023 at 3:34 p.m. | |
| Citation: | See how to cite this resource |
| Sharing Status: | Public |
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| Views: | 320 |
| Downloads: | 187 |
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Abstract
The Zhangye basin is in the middle reaches of the Heihe River, northwestern China. Heavy abstraction of groundwater since the 1970s in the area is for agricultural, industrial and drinking water supplies and has led to a substantial decline in the potentiometric surface. A three-dimensional regional numerical groundwater flow model, calibrated under transient conditions, has been developed and used to predict the drawdown for the period from 2000 to 2030 under two different groundwater management scenarios.
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Additional Metadata
| Name | Value |
|---|---|
| DOI | 10.1007/s00254-006-0620-7 |
| Depth | 500 |
| Scale | 10 001 - 100 000 km² |
| Layers | 5 |
| Purpose | Groundwater resources |
| GroMoPo_ID | 315 |
| IsVerified | True |
| Model Code | Feflow |
| Model Link | https://doi.org/10.1007/s00254-006-0620-7 |
| Model Time | 2000-2030 |
| Model Year | 2007 |
| Model Authors | Wen, XH; Wu, YQ; Lee, LJE; Su, JP; Wu, J |
| Model Country | China |
| Data Available | Report/paper only |
| Developer Email | wenxiaohu@gmail.com |
| Dominant Geology | Unconsolidated sediments |
| Developer Country | Peoples R China |
| Publication Title | Groundwater flow modeling in the zhangye basin, northwestern china |
| Original Developer | No |
| Additional Information | |
| Integration or Coupling | None of the above |
| Evaluation or Calibration | Dynamic water levels |
| Geologic Data Availability | No |
How to Cite
This resource is shared under the Creative Commons Attribution CC BY.
http://creativecommons.org/licenses/by/4.0/
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