<p>This data includes two core indicators: pore water storage and dynamic water storage in the Quaternary sediments of Kyrgyzstan. The pore water storage of the Quaternary sediments includes 9 hydrogeological areas and 24 artesian water basins including Chu-Talas, Isekhusky, Narensky, and Ako-Arpensky. Dynamic water storage includes 27 major groundwater basins such as Chu River, Talas River, and Issyk Lake. The two types of indicators jointly reflect the spatial distribution characteristics of pore water resources. Most of the high-value areas are concentrated in large river basins and basins, while the storage in mountainous and marginal areas is relatively limited. </p>
| data size | 44.0 KiB |
|---|---|
| data format | .xlsx format |
| Coordinate system | |
| Projection | no |
The data comes from the monograph "ˇ одн ы е р е сур с ы Кы ргызс т а н а н а с о в р е м е н н о м а н т апе"(Current Situation of Water Resources in Kyrgyzstan) published in 2007 and provided by the National Institute of Hydrology of Kyrgyzstan.
After digital scanning, OCR recognition, and manual verification.
The data content has not been changed.
| # | number | name | type |
| 1 | 2010DFA92720 | Central Asia | International cooperation project of the Ministry of science and technology |
This work is licensed under a
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Commons Attribution 4.0 International License.
| # | title | file size |
|---|---|---|
| 1 | 表3-1吉国第四纪沉积层孔隙水贮量.xls | 22.5 KiB |
| 2 | 表3-2吉国第四纪沉积层孔隙水动态贮量.xls | 21.5 KiB |
pore water storage Quaternary sediments dynamic water storage
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