本数据包含吉尔吉斯斯坦第四纪沉积层孔隙水贮量与动态贮水量两类核心指标。第四纪沉积层孔隙水贮量包含楚—塔拉斯、伊塞克湖斯基、纳伦斯基、阿克奥—阿尔贫斯基等9个水文地质区和24个自流水流域。动态贮水量包含楚河、塔拉斯河、伊塞克湖等27个主要地下水流域，。两类指标共同反映了孔隙水资源的空间分布特征，高值区多集中在大型河流流域及盆地，而山区及边缘地带贮量相对有限。
", "ds_source": "数据来自专著《Водные ресурсы Кыргызстана на современном этапе》（吉国水资源现状） 2007出版，由吉尔吉斯斯坦国立水文研究所提供。
", "ds_process_way": "经过数字化扫描，OCR识别、人工核对整理。
", "ds_quality": "数据内容未做改动。
", "ds_acq_start_time": null, "ds_acq_end_time": null, "ds_acq_place": "", "ds_acq_lon_east": null, "ds_acq_lat_south": null, "ds_acq_lon_west": null, "ds_acq_lat_north": null, "ds_acq_alt_low": null, "ds_acq_alt_high": null, "ds_share_type": "login-access", "ds_total_size": 45056, "ds_files_count": 2, "ds_format": ".xlsx格式", "ds_space_res": "无", "ds_time_res": "", "ds_coordinate": "无", "ds_projection": "无", "ds_thumbnail": "41827a69-acb0-44ee-b4f4-f96861ddbec4.png", "ds_thumb_from": 2, "ds_ref_way": "", "paper_ref_way": "", "ds_ref_instruction": "", "ds_from_station": null, "organization_id": "a5877b42-96ea-4f13-af7e-246f355413d6", "doi_value": "", "subject_codes": [ "170.50" ], "quality_level": 1, "publish_time": "2025-05-14 19:05:27", "first_publish_time": null, "last_updated": "2025-05-14 19:05:27", "protected": false, "protected_to": null, "lang": "zh", "cstr": "33110.11.ariddc.00610", "license": null, "extra": null, "files_shape": [ { "name": "表3-1吉国第四纪沉积层孔隙水贮量.xls", "size": 23040, "is_dir": false }, { "name": "表3-2吉国第四纪沉积层孔隙水动态贮量.xls", "size": 22016, "is_dir": false } ], "features": null, "data_level": 0, "i18n": { "en": { "title": "Pore water storage in Quaternary sediments of Kyrgyzstan in 2007", "ds_abstract": "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.
", "ds_source": "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.
", "ds_process_way": "After digital scanning, OCR recognition, and manual verification.
", "ds_quality": "The data content has not been changed.
", "ds_format": ".xlsx format", "ds_projection": "no", "ds_space_res": "no" } }, "license_type": null, "doi_reg_from": "reg_local", "cstr_reg_from": "reg_local", "doi_not_reg_reason": null, "cstr_not_reg_reason": null, "is_paper_in_submitting": false, "ds_topic_tags": [ "孔隙水贮量", "第四纪沉积层", "动态贮水量" ], "ds_subject_tags": [ "地质学" ], "ds_class_tags": [], "ds_locus_tags": [ "吉尔吉斯斯坦" ], "ds_time_tags": [ 2007 ], "ds_contributors": [ "陈曦" ], "ds_meta_authors": [ "李锦" ], "ds_managers": [ "李锦" ], "category": "水文" }