{
    "created": "2020-11-10 08:56:37",
    "updated": "2026-05-01 07:15:15",
    "id": "1457b02f-5cf1-4871-8d7e-aa874074e7d3",
    "version": null,
    "ds_topic": null,
    "title_cn": "2016-2020年黄土丘陵沟壑区第一副区辛店沟流域育林沟不同坡度径流场观测数据集",
    "title_en": "Observation data set of runoff field with different slopes in Yulin Gully Watershed of xindiangou watershed in the first sub region of Loess Hilly and gully region from 2016 to 2020",
    "ds_abstract": "<p>本数据集为2016-2020年黄土丘陵沟壑区第一副区辛店沟流域育林沟不同坡度径流场数据。对育林沟不同坡度径流场产生径流的次降水量、径流量、泥沙量进行观测，对比不同坡度的减水减沙效益。径流场情况见育林沟不同坡度径流场2016-2020年情况说明。数据包括育林沟不同坡度径流场逐次径流泥沙测验成果表、土壤含水率实测成果表，径流场基本情况见《育林沟不同坡度径流场2016-2020年情况说明》</p>",
    "ds_source": "<p>人工观测</p>",
    "ds_process_way": "<p>1.雨量观测：育林沟不同坡度类型径流小区降水量采用试验场雨量站的资料。 2.泥沙取样及处理：径流、泥沙采用不同的观测设施，有分水箱、径流池，分水箱、径流池在降水结束、径流终止后立即读取径流池水位，根据分水箱、径流池面积、水位计算径流量；将分水箱、径流池泥水搅拌均匀取泥沙样，样品处置采用置换法。 3.土壤含水率：在具有代表性的固定地点，去除表层杂草后，在30cm深度取样，用烘干（称重）法测定。</p>",
    "ds_quality": "<p>观测数据整编录入过程中经过四级人工校核，分别是制表、初校、复校、审核，以确保数据质量。                        </p>",
    "ds_acq_start_time": "2016-01-01 00:00:00",
    "ds_acq_end_time": "2020-12-31 00:00:00",
    "ds_acq_place": "陕西省榆林市绥德县辛店沟流域",
    "ds_acq_lon_east": 110.29666666666667,
    "ds_acq_lat_south": 37.49472222222222,
    "ds_acq_lon_west": 110.2775,
    "ds_acq_lat_north": 37.516666666666666,
    "ds_acq_alt_low": 2.0,
    "ds_acq_alt_high": null,
    "ds_share_type": "apply-access",
    "ds_total_size": 171398,
    "ds_files_count": 9,
    "ds_format": "xls，doc，pdf",
    "ds_space_res": null,
    "ds_time_res": "分、日、次",
    "ds_coordinate": "WGS84",
    "ds_projection": "",
    "ds_thumbnail": "1457b02f-5cf1-4871-8d7e-aa874074e7d3.jpg",
    "ds_thumb_from": 2,
    "ds_ref_way": "黄河水土保持绥德治理监督局（绥德水土保持科学试验站），2016-2020年黄土丘陵沟壑区第一副区辛店沟流域育林沟不同坡度径流场观测数据集，国家冰川冻土沙漠科学数据中心(www.ncdc.ac.cn)，2020，doi：10.12072/ncdc.HWSDZhan.db0066.2020",
    "paper_ref_way": "",
    "ds_ref_instruction": "",
    "ds_from_station": null,
    "organization_id": "f447b2e7-0b54-4601-8d49-0164f2a3fd9a",
    "ds_serv_man": "敏玉芳",
    "ds_serv_phone": "09314967597",
    "ds_serv_mail": "myf@lzb.ac.cn",
    "doi_value": "",
    "subject_codes": null,
    "quality_level": 3,
    "publish_time": "2021-10-27 21:19:14",
    "last_updated": "2021-10-27 21:19:14",
    "protected": false,
    "protected_to": null,
    "lang": "zh",
    "cstr": "11738.11.ncdc.HWSDZhan.2020.101",
    "i18n": {
        "en": {
            "title": "Observation data set of runoff field with different slopes in Yulin Gully Watershed of xindiangou watershed in the first sub region of Loess Hilly and gully region from 2016 to 2020",
            "ds_format": "",
            "ds_source": "<pre><code>                                              &lt;p&gt;Manual timing observation&lt;/p&gt;\n</code></pre>",
            "ds_quality": "<pre><code>                                                      &lt;p&gt;In the process of compilation and input of observation data, there are four levels of manual verification, including tabulation, primary calibration, recheck and audit, so as to ensure the data quality. &lt;/p&gt;\n</code></pre>",
            "ds_ref_way": "                        \nSuide administration and Supervision Bureau of soil and water conservation of the Yellow River (Suide scientific experimental station of soil and water conservation), 2016-2020 observation data set of runoff field at different slopes in Yulingou basin, the first sub area of Loess Hilly and gully region, national glacier, frozen soil and desert scientific data center (www.ncdc. Ac.cn), 2020, DOI: 10.12072/ncdc.hwsdzhan.db0066.2020",
            "ds_abstract": "<pre><code> &lt;p&gt;This data set is the runoff field data of different slopes of Yulin gully in xindiangou watershed of the first sub region of Loess Hilly and gully region from 2016 to 2020. The precipitation, runoff and sediment yield of runoff generated by runoff field with different slopes in Yulin gully were observed, and the benefits of water and sediment reduction with different slopes were compared. For runoff and flow field, please refer to the description of runoff field in Yulin ditch from 2016 to 2020. For the basic situation of runoff and flow field, see the description of runoff field with different slopes in Yulin ditch from 2016 to 2020&lt;/p&gt;\n</code></pre>",
            "ds_time_res": "分、日、次",
            "ds_acq_place": "Xindiangou watershed, Suide County, Yulin City, Shaanxi Province",
            "ds_space_res": "",
            "ds_projection": "",
            "ds_process_way": "<pre><code>                                              &lt;p&gt;1. Rainfall observation: the observation instruments for precipitation include SM1 ordinary rain gauge with diameter of 20cm and dsj2 siphon self recording rain gauge. The precipitation of runoff plots with different slopes is based on the data of rainfall stations in the test site.\n</code></pre>\n<ol>\n<li>Sediment sampling and treatment: different observation facilities are adopted for runoff and sediment, including triangular weir, triangular groove, water distribution tank and runoff pool. Sand ocean is collected by triangular weir and triangular groove in the process of runoff generation; the water level of runoff pool is read immediately after precipitation and runoff is terminated, and runoff is calculated according to the area and water level of water distribution tank and runoff pool The sediment sample (500cm3) was taken by mixing water evenly, and the replacement method was used for sample disposal.</li>\n<li>Soil moisture content: in a representative fixed site, after removing the surface weeds, samples were taken at a depth of 30 cm and determined by drying (weighing) method. </p></li>\n</ol>",
            "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": [
        "次降水强度",
        "含沙量",
        "冲刷量",
        "径流深",
        "径流系数",
        "径流",
        "次降水量"
    ],
    "ds_subject_tags": [],
    "ds_class_tags": [],
    "ds_locus_tags": [
        "辛店沟",
        "绥德",
        "榆林"
    ],
    "ds_time_tags": [
        2016,
        2017,
        2018,
        2019,
        2020
    ],
    "ds_contributors": [
        {
            "true_name": "黄河水土保持绥德治理监督局（绥德水土保持科学试验站）",
            "email": "hhstbcsdzljdj@163.com",
            "work_for": "黄河水土保持绥德治理监督局（绥德水土保持科学试验站）",
            "country": "中国"
        }
    ],
    "ds_meta_authors": [
        {
            "true_name": "雷欣",
            "email": "hhstbcsdzljdj@163.com",
            "work_for": "黄河水土保持绥德治理监督局（绥德水土保持科学试验站）",
            "country": "中国"
        }
    ],
    "ds_managers": [
        {
            "true_name": "郭玉梅",
            "email": "hhstbcsdzljdj@163.com",
            "work_for": "黄河水土保持绥德治理监督局（绥德水土保持科学试验站）",
            "country": "中国"
        },
        {
            "true_name": "黄河水土保持绥德治理监督局（绥德水土保持科学试验站）",
            "email": "hhstbcsdzljdj@163.com",
            "work_for": "黄河水土保持绥德治理监督局（绥德水土保持科学试验站）",
            "country": "中国"
        }
    ],
    "category": "水土保持"
}