本数据为河西内陆河流域祁连山区地下水统计数据。数据为excel表格数据，共计四个表格，分别为内陆河流域山丘地下水资源量、内陆河流域平原区地下水资源量、内陆河流域分河地下水资源总量和内陆河流域多年平均地下水可开采量，其中内陆河流域分别为：疏勒河、黑河和石羊河;监测指标如下：内陆河流域山丘地下水资源量（河流名、河川基流量、侧向流出量、潜水蒸发量、开采消耗量、地下水资源量）；内陆河流域平原区地下水资源量（河名、降水渗入补给量、山前侧向补给量、地表水体渗漏补给量、井灌回归补给量、总补给量、地下水资源量）；内陆河流域分河地下水资源总量（河名、山丘总补给量、平原总补给量、总补给量、平原余山区重复计算量、地下水资源量、地表水与地下水重复计算量、纯地下水资源量）；内陆河流域分河多年平均地下水可开采量（河名、山丘区总补给量、平原与山丘区重复计算量、地下水资源量、地表水与地下水重复计算量、纯地下水资源量）。
", "ds_source": "数据来源于甘肃出版社出版的《甘肃祁连山国家级自然保护区志》。", "ds_process_way": "
纸质数据数字化、多年数据求均值
", "ds_quality": "数据质量良好
", "ds_acq_start_time": "1956-01-01 00:00:00", "ds_acq_end_time": "1997-12-31 00:00:00", "ds_acq_place": "祁连山自然保护区", "ds_acq_lon_east": 103.76472222222222, "ds_acq_lat_south": 36.49916666666667, "ds_acq_lon_west": 97.39277777777778, "ds_acq_lat_north": 39.465, "ds_acq_alt_low": null, "ds_acq_alt_high": null, "ds_share_type": "login-access", "ds_total_size": 13005, "ds_files_count": 2, "ds_format": "Excel", "ds_space_res": null, "ds_time_res": "年", "ds_coordinate": "无", "ds_projection": "", "ds_thumbnail": "d93d148d-cdff-4ee5-a1a4-1542ebd291cc.jpg", "ds_thumb_from": 2, "ds_ref_way": "", "paper_ref_way": "", "ds_ref_instruction": "", "ds_from_station": null, "organization_id": "9c4867b1-5cb1-4de0-abeb-df42547bf41e", "ds_serv_man": "李红星", "ds_serv_phone": "0931-4967592", "ds_serv_mail": "ncdc@lzb.ac.cn", "doi_value": "", "subject_codes": [ "170.4510" ], "quality_level": 3, "publish_time": "2021-01-29 14:46:15", "last_updated": "2025-04-29 15:07:46", "protected": false, "protected_to": null, "lang": "zh", "cstr": "11738.11.ncdc.Westdc.2021.833", "i18n": { "en": { "title": "Groundwater statistics of Qilian Mountain Area in Hexi Inland River Basin", "ds_format": "Excel", "ds_source": "The data comes from the chronicle of Qilian Mountain National Nature Reserve in Gansu Province published by Gansu publishing house. The indicators of each data table are as follows: the amount of mountain groundwater resources in the Inland River Basin (river name, river base flow, lateral outflow, phreatic water evaporation, exploitation consumption, groundwater resources); the amount of groundwater resources in the plain area of the Inland River Basin (river name, precipitation infiltration recharge, piedmont lateral recharge, surface water leakage recharge, well irrigation return recharge, total recharge) The total amount of groundwater resources (river name, total recharge of hills, total recharge of plain, total recharge, repeated calculation of remaining mountain area in plain, groundwater resources, repeated calculation of surface water and groundwater, and pure groundwater resources) in inland river basin; the average annual exploitable amount of groundwater (river name, total recharge of hills, total recharge of plain, total recharge of plain, repeated calculation of surface water and groundwater, and pure groundwater resources) in inland river basin In plain and hilly areas, the amount of repeated calculation, the amount of groundwater resources, the amount of repeated calculation of surface water and groundwater, and the amount of pure groundwater resources).
", "ds_quality": "Good data quality
", "ds_ref_way": "", "ds_abstract": "This data is the statistical data of groundwater in Qilian mountain area of Hexi inland river basin. The data is excel data, with a total of four tables, which are respectively the amount of groundwater resources in hilly area of inland river basin, the amount of groundwater resources in plain area of inland river basin, the total amount of groundwater resources in different rivers of inland river basin, and the average annual exploitable amount of groundwater in inland river basin; The monitoring indicators are as follows: the amount of groundwater resources in the hills of the Inland River Basin (river name, river base flow, lateral outflow, phreatic water evaporation, exploitation consumption and groundwater resources); the amount of groundwater resources in the plain area of the Inland River Basin (river name, precipitation infiltration recharge, lateral recharge in front of the mountain, surface water leakage recharge, well irrigation return recharge, total recharge and groundwater recharge) The total amount of groundwater resources (river name, total recharge of hill, total recharge of plain, total recharge, repeated calculation of remaining mountain area in plain, groundwater resources, repeated calculation of surface water and groundwater, and pure groundwater resources) in inland river basin; the average annual exploitable amount of groundwater in inland river basin (river name, total recharge of hill, total recharge of plain and plain) In hilly area, repeated calculation quantity, groundwater resources quantity, surface water and groundwater repeated calculation quantity, pure groundwater resources quantity).
", "ds_time_res": "年", "ds_acq_place": "Qilian Mountains Nature Reserve", "ds_space_res": "", "ds_projection": "", "ds_process_way": "Digitization of paper data and mean value of multi-year data
", "ds_ref_instruction": "" } }, "submit_center_id": "ncdc", "data_level": 0, "license_type": "CC BY 4.0", "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": [ "水文", "祁连山", "降水资源量", "年径流量" ], "ds_subject_tags": [ "自然地理学" ], "ds_class_tags": [], "ds_locus_tags": [ "祁连山", "黑河", "疏勒河", "祁连山自然保护区", "石羊河" ], "ds_time_tags": [ 1956, 1957, 1958, 1959, 1960, 1961, 1962, 1963, 1964, 1965, 1966, 1967, 1968, 1969, 1970, 1971, 1972, 1973, 1974, 1975, 1976, 1977, 1978, 1979, 1980, 1981, 1982, 1983, 1984, 1985, 1986, 1987, 1988, 1989, 1990, 1991, 1992, 1993, 1994, 1995, 1996, 1997 ], "ds_contributors": [ { "true_name": "吴立宗", "email": "wulizong@pric.org.cn", "work_for": "国家极地科学数据中心", "country": "中国" } ], "ds_meta_authors": [ { "true_name": "盖春梅", "email": "Gechm@lzb.ac.cn", "work_for": "中国科学院西北生态环境资源研究院", "country": "中国" } ], "ds_managers": [ { "true_name": "李红星", "email": "lihongxing@lzb.ac.cn", "work_for": "中国科学院西北生态环境资源研究院", "country": "中国" } ], "category": "水文" }