{
    "created": "2022-09-08 11:29:54",
    "updated": "2026-04-28 11:36:19",
    "id": "b82103b6-9027-4eeb-9282-53feaf8fe73d",
    "version": 8,
    "ds_topic": null,
    "title_cn": "柴达木盆地产水量和水源涵养量数据集（1980-2018年）",
    "title_en": "Data set of water consumption and water conservation in Chaidamu Basin (1980-2018)",
    "ds_abstract": "<p>&emsp;&emsp;本数据是研究团队利用柴达木盆地土地利用、气象、土壤、地形等数据，采用InVEST模型定量评估柴达木盆地1980-2018年生态系统产水量，基于产水量综合考虑土壤渗透性、地类的地表径流差异和地形等因素评估水源涵养量，空间分辨率为1km，单位为mm。",
    "ds_source": "<p>&emsp;&emsp;土地利用数据、气象数据、土壤数据和地形数据等。",
    "ds_process_way": "<p>&emsp;&emsp;基于柴达木盆地土地利用数据，结合气象数据、土壤数据、地形数据等， 运用InVEST模型产水量模块，对1980–2018年柴达木盆地产水量进行定量评估，基于产水量综合考虑土壤渗透性、地类的地表径流差异和地形等因素评估水源涵养量。",
    "ds_quality": "<p>&emsp;&emsp;根据《青海省水资源公报》中柴达木盆地多年平均总径流量，扣除冰川补给部分，与柴达木盆地1980–2018年产水量模拟结果进行对比，确定Z值，通过误差计算，发现InVEST模型对于产水量的模拟结果比较准确，相对误差小于5%。基于产水量综合考虑土壤渗透性、地类的地表径流差异和地形等因素评估水源涵养量。",
    "ds_acq_start_time": "1980-01-01 00:00:00",
    "ds_acq_end_time": "2018-12-31 00:00:00",
    "ds_acq_place": "柴达木盆地",
    "ds_acq_lon_east": 99.25,
    "ds_acq_lat_south": 35.0,
    "ds_acq_lon_west": 90.25,
    "ds_acq_lat_north": 39.31666666666667,
    "ds_acq_alt_low": null,
    "ds_acq_alt_high": null,
    "ds_share_type": "login-access",
    "ds_total_size": 11756568,
    "ds_files_count": 3,
    "ds_format": "tif",
    "ds_space_res": "1km",
    "ds_time_res": "年",
    "ds_coordinate": "WGS84",
    "ds_projection": "",
    "ds_thumbnail": "b82103b6-9027-4eeb-9282-53feaf8fe73d.png",
    "ds_thumb_from": 0,
    "ds_ref_way": "",
    "paper_ref_way": "",
    "ds_ref_instruction": "",
    "ds_from_station": null,
    "organization_id": "4851e874-eafc-4879-812b-ffbdd825e967",
    "ds_serv_man": "敏玉芳",
    "ds_serv_phone": "0931-4967596",
    "ds_serv_mail": "ncdc@lzb.ac.cn",
    "doi_value": "10.12072/ncdc.Hydro.db2443.2022",
    "subject_codes": [
        "170.55"
    ],
    "quality_level": 3,
    "publish_time": "2022-09-29 10:34:57",
    "last_updated": "2025-04-29 15:32:38",
    "protected": false,
    "protected_to": null,
    "lang": "zh",
    "cstr": "11738.11.ncdc.Hydro.db2443.2022",
    "i18n": {
        "en": {
            "title": "Data set of water consumption and water conservation in Chaidamu Basin (1980-2018)",
            "ds_format": "TIF",
            "ds_source": "<p>&emsp; Land use data, meteorological data, soil data and topographic data.",
            "ds_quality": "<p>&emsp; According to the annual average total runoff of the Qaidam Basin in the Qinghai water resources bulletin, after deducting the glacier recharge, the Z value is determined by comparing the simulation results of the annual water production of the Qaidam Basin from 1980 to 2018. Through error calculation, it is found that the simulation results of the invest model for water production are relatively accurate, and the relative error is less than 5%. Based on the water yield, the water conservation capacity is evaluated by comprehensively considering the factors such as soil permeability, surface runoff difference of land types and topography.",
            "ds_ref_way": "",
            "ds_abstract": "<p>  This data is used by the research team to quantitatively evaluate the ecosystem water yield of the Qaidam Basin from 1980 to 2018 by using the invest model based on the data of land use, meteorology, soil, topography, etc. of the Qaidam Basin. Based on the water yield, the water conservation capacity is evaluated by comprehensively considering the factors such as soil permeability, surface runoff difference of land types and land shape. The spatial resolution is 1km, and the unit is mm.</p>",
            "ds_time_res": "年",
            "ds_acq_place": "Qaidam Basin",
            "ds_space_res": "1km",
            "ds_projection": "",
            "ds_process_way": "<p>&emsp; Based on the land use data of the Qaidam Basin, combined with meteorological data, soil data, topographic data, etc., the water yield module of the invest model is used to quantitatively evaluate the water yield of the Qaidam Basin from 1980 to 2018, and the water conservation capacity is evaluated based on the water yield by comprehensively considering the soil permeability, the surface runoff difference of different types and the terrain.",
            "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": [
        "InVEST模型",
        "产水量",
        "水源涵养量"
    ],
    "ds_subject_tags": [
        "水文学"
    ],
    "ds_class_tags": [],
    "ds_locus_tags": [
        "柴达木盆地"
    ],
    "ds_time_tags": [
        1980,
        1990,
        1995,
        2000,
        2005,
        2010,
        2015,
        2018
    ],
    "ds_contributors": [
        {
            "true_name": "朱高峰",
            "email": "zhugf@lzu.edu.cn",
            "work_for": "兰州大学",
            "country": "中国"
        }
    ],
    "ds_meta_authors": [
        {
            "true_name": "崔霞",
            "email": "xiacui@lzu.edu.cn",
            "work_for": "兰州大学",
            "country": "中国"
        }
    ],
    "ds_managers": [
        {
            "true_name": "朱高峰",
            "email": "zhugf@lzu.edu.cn",
            "work_for": "兰州大学",
            "country": "中国"
        }
    ],
    "category": "生态"
}