本数据集为2023年王茂沟流域径流站径流、泥沙观测数据，通过径流站测流断面水位观测，泥沙取样，计算产流时的径流、泥沙量。数据包括王茂沟径流站测流断面图、洪水水文要素摘录表、逐次洪水测验成果表、逐日平均流量表、逐日平均含沙量表、逐日平均输沙率表。径流站情况见《王茂沟流域2023年情况说明》。\n
", "ds_source": "人工定时观测
", "ds_process_way": "1.水位观测：王茂沟径流站利用建筑物侧壁上的水尺进行水位测定，非汛期每日8时观测一次，如有降雨，日水位变化缓慢时8时、20时观测两次；日水位变化较大或出现缓慢的峰谷时按2时、8时、14时、20时观测四次。汛期水位变化剧烈时按6分钟的倍数观测。 2.测流方式：平水时采用三角槽测流；水位高于三角槽时，在矩形溢洪道采用浮标法测流，浮标系数采用黄委子洲径流试验站浮标试验结果。 3.泥沙取样及处理：测流断面泥沙采用中泓浮标法取样，取沙次数取决于洪水水位变化的次数，洪峰时为控制含沙量变化而增加取样次数。样品处理采用置换法。
", "ds_quality": "由专业技术人员进行人工观测；数据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。
", "ds_acq_start_time": "2023-01-01 00:00:00", "ds_acq_end_time": "2023-12-31 00:00:00", "ds_acq_place": "陕西省榆林市绥德县王茂沟流域", "ds_acq_lon_east": 110.37944444444443, "ds_acq_lat_south": 37.571111111111115, "ds_acq_lon_west": 110.34277777777777, "ds_acq_lat_north": 37.59444444444445, "ds_acq_alt_low": 2.0, "ds_acq_alt_high": null, "ds_share_type": "apply-access", "ds_total_size": 532026, "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": "fddac88a-bdd2-4199-9633-8dbff9a49711.jpg", "ds_thumb_from": 0, "ds_ref_way": "", "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": [], "quality_level": 3, "publish_time": "2024-09-23 14:50:48", "last_updated": "2024-09-23 14:50:48", "protected": false, "protected_to": null, "lang": "zh", "cstr": "11738.11.NCDC.HWSDZHAN.DB6582.2024", "i18n": { "en": { "title": "Observation dataset of runoff and sediment in Wangmaogou watershed, the first sub area of loess hilly and gully region in 2023", "ds_format": "", "ds_source": "Manual timing observation",
"ds_quality": "Manual observation shall be conducted by professional technicians; during data entry, four levels of manual verification shall be conducted, including tabulation, primary calibration, re calibration and audit, so as to ensure data quality.\n
\nThis dataset is the runoff and sediment observation data of Wangmaogou watershed runoff station in 2023. By observing the water level of the runoff station measurement section, taking sediment samples, and calculating the runoff and sediment volume during runoff production. The data includes the flow section diagram of Wangmaogou runoff station, the extracted table of flood hydrological elements, the results of successive flood tests, the daily average flow table, the daily average sediment concentration table, and the daily average sediment transport rate table. The situation of the runoff station can be found in the \"Explanation of the Situation in Wangmaogou Basin in 2023\".\n
", "ds_time_res": "分、日、次", "ds_acq_place": "Wangmaogou watershed, Suide County, Yulin City, Shaanxi Province", "ds_space_res": "", "ds_projection": "", "ds_process_way": "1. The water level observation method of runoff station is: wangmaogou runoff station uses the water gauge on the side wall of the building to measure the water level. In the non flood season, the water level is observed once a day at 8:00 and 20:00 in case of rainfall; the observation is conducted four times at 2:00, 8:00, 14:00 and 20:00 when the daily water level changes greatly or has a slow peak and valley. When the water level changes violently in flood season, the observation shall be made in multiples of 6 minutes.\n2.The flow measurement method of wangmaozhuang runoff station: the calibrated natural section observation by manual arrangement is adopted, and the calibrated flow formula is used for flow calculation.\n3.Sediment sampling and treatment: the midstream buoy method is used to sample the sediment at the flow measurement section. The frequency of sediment sampling depends on the frequency of flood water level change, and the sampling frequency is increased to control the change of sediment concentration at flood peak. The sample was treated by displacement method.\n",
"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": [
"径流模数",
"径流系数",
"输沙率",
"水位",
"侵蚀模数",
"流量",
"含沙量",
"径流深度",
"径流量",
"土壤流失量"
],
"ds_subject_tags": [],
"ds_class_tags": [],
"ds_locus_tags": [
"榆林",
"绥德",
"王茂沟",
"陕西省"
],
"ds_time_tags": [
2023
],
"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": "崔钰",
"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": "麦旭东",
"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": "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"
},
{
"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"
}
],
"category": "水土保持"
}