{
    "created": "2019-10-10 15:55:05",
    "updated": "2026-05-08 23:05:46",
    "id": "80c9d9d4-5a1c-4f76-826c-161c17389431",
    "version": null,
    "ds_topic": null,
    "title_cn": "2016-2019年藏东南扎木弄巴滑坡观测数据",
    "title_en": "Observation data of Zhamunongba landslide in Southeastern Tibet from 20016 to 2019",
    "ds_abstract": "<p>\n本数据集为2016-2019年藏东南扎木弄巴滑坡观测数据，该站位于西藏自治区波密县易贡乡，易贡乡扎木弄沟位于南巴迦瓦峰北北西侧，易贡藏布左岸，地势上西高东低，其地貌类型属于高山地貌，流域面积29.4km2，区域内地质构造的隆升显著，扎木弄沟地处易贡-通麦-波密断裂带的相对隆升区的边缘，这些隆升区由一系列的横向构造影响，区域成为周期或准周期滑坡泥石流灾害的易发区。该观测站详细记录滑坡相关数据，数据由布设现场的翻斗式降雨量传感器、土壤温度传感器、空隙水压力传感器、含水量传感器、水势传感器、振动传感器测得，采集频率10分钟/条，由CR1000数据采集器取得原始数据，土壤温度、孔隙水压力、含水量、水势、振动这些参数采用日平均数据并整理，降雨数据采用日累计数据并整理。\n</p>\n\n<p>\n站点名称：扎木弄巴滑坡观测站,经纬度：94 °56′54,30°11′13,海拔高程：2550米数据内容：降雨量单位为毫米（mm），土壤温度单位为摄氏度（℃），孔隙水压力单位为千帕（Kpa），含水量单位为容积率（m3/m3），水势单位为帕（pa）， 振动单位为加速度(g）\n</p>",
    "ds_source": "<p>自动采集</p>",
    "ds_process_way": "<p>原始数据由现场仪器自动采集，每十分钟采集一次，由专业人员定期进行收集和汇总，土壤温度、孔隙水压力、含水量、水势、振动采用日平均数据，雨量数据采用累计降雨量数据并整理，后加工为数据集产品</p>",
    "ds_quality": "<p>本数据在获取处理各阶段均有专业人员负责，数据质量良好。</p>",
    "ds_acq_start_time": "2016-08-11 00:00:00",
    "ds_acq_end_time": "2019-08-27 00:00:00",
    "ds_acq_place": "西藏自治区波密县易贡乡",
    "ds_acq_lon_east": 94.96194444444444,
    "ds_acq_lat_south": 30.844444444444445,
    "ds_acq_lon_west": 94.93194444444445,
    "ds_acq_lat_north": 30.192777777777778,
    "ds_acq_alt_low": 2000.0,
    "ds_acq_alt_high": 3000.0,
    "ds_share_type": "apply-access",
    "ds_total_size": 176506,
    "ds_files_count": 2,
    "ds_format": "excel",
    "ds_space_res": null,
    "ds_time_res": "日",
    "ds_coordinate": "WGS84",
    "ds_projection": "",
    "ds_thumbnail": "80c9d9d4-5a1c-4f76-826c-161c17389431.jpg",
    "ds_thumb_from": 2,
    "ds_ref_way": "陈宁生, 丁海涛, 邓明枫，2016-2019年藏东南扎木弄巴滑坡观测数据，国家冰川冻土沙漠科学数据中心(www.ncdc.ac.cn)，2019，doi：10.12072/ncdc.BoMi.db0001.2020",
    "paper_ref_way": "",
    "ds_ref_instruction": "在使用数据时，请明显标注“本数据来自青藏高原冰冻圈观测研究站”",
    "ds_from_station": null,
    "organization_id": "81514787-dc21-4e92-a0f4-fe23e24502f5",
    "ds_serv_man": "李红星",
    "ds_serv_phone": "0931-4967592",
    "ds_serv_mail": "lihongxing@lzb.ac.cn",
    "doi_value": "",
    "subject_codes": null,
    "quality_level": 3,
    "publish_time": "2020-12-24 11:50:16",
    "last_updated": "2023-05-16 17:35:14",
    "protected": false,
    "protected_to": null,
    "lang": "zh",
    "cstr": "11738.11.ncdc.BoMi.2020.17",
    "i18n": {
        "en": {
            "title": "Observation data of Zhamunongba landslide in Southeastern Tibet from 20016 to 2019",
            "ds_format": "",
            "ds_source": "<p>Automatic acquisition</p>",
            "ds_quality": "<p>The data were acquired and processed by professionals at all stages of the process, and the quality of the data was good. </p>",
            "ds_ref_way": "Chen Ningsheng, Ding Haitao, Deng Mingfeng, observation data of Zhamunongba landslide in Southeastern Tibet, 2016-2019, national glacier frozen soil desert scientific data center（ www.ncdc.ac.cn )，2019，doi：10.12072/ ncdc.BoMi.db0001.2020",
            "ds_abstract": "<p>\nThis data set is the observation data of Zhamunongba landslide in Southeastern Tibet from 2016 to 2019. The station is located in Yigong Township, Bomi County, Tibet Autonomous Region. Zhamunonggou is located in the northwest of nanbajiawa peak and the left bank of Yigong Zangbu. The terrain is high in the West and low in the East. Its geomorphic type belongs to alpine landform, with a drainage area of 29.4km2. The geological structure in the area has been significantly uplifted. Zhamunonggou is located in Yigong Tongmai- These uplifted areas are affected by a series of lateral structures and become the prone areas of periodic or quasi periodic landslides and debris flows. The observation station records landslide related data in detail. The data are measured by bucket type rainfall sensor, soil temperature sensor, pore water pressure sensor, water content sensor, water potential sensor and vibration sensor on the site. The collection frequency is 10 minutes / piece. The original data of soil temperature, pore water pressure, water content, water potential and vibration are obtained by CR1000 data collector Daily average data is used for some parameters, and daily cumulative data is used for rainfall data.\n</p>\n<p>\nStation Name: zhamunongba landslide observation station, longitude and latitude: 94 ° 56 ′ 54,30 ° 11 ′ 13, altitude: 2550m data content: rainfall unit is mm, soil temperature unit is centigrade (℃), pore water pressure unit is kPa (kPa), water content unit is volume ratio (m3 / m3), unit of water potential is pa (PA), unit of vibration is acceleration (g)\n</p>",
            "ds_time_res": "日",
            "ds_acq_place": "Yigong Township, Bomi County, Tibet Autonomous Region",
            "ds_space_res": "",
            "ds_projection": "",
            "ds_process_way": "<p>The original data is collected automatically by field instruments every 10 minutes, and collected and summarized by professionals regularly. The daily average data of soil temperature, pore water pressure, water content, water potential and vibration are used, and the rainfall data are processed by accumulated rainfall data, and then processed into data set products</p>",
            "ds_ref_instruction": "                    \nWhen using the data, please clearly mark \"this data is from the cryosphere observation and research station of Qinghai Tibet Plateau\""
        }
    },
    "submit_center_id": "ncdc",
    "data_level": 0,
    "license_type": "https://creativecommons.org/licenses/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": [
        "滑坡",
        "土壤温度",
        "降雨量",
        "含水量",
        "水势",
        "振动",
        "孔隙水压力"
    ],
    "ds_subject_tags": [
        "自然地理学"
    ],
    "ds_class_tags": [],
    "ds_locus_tags": [
        "易贡乡",
        "西藏自治区",
        "波密县"
    ],
    "ds_time_tags": [
        2016,
        2017,
        2018,
        2019
    ],
    "ds_contributors": [
        {
            "true_name": "陈宁生",
            "email": "chennsh@imde.ac.cn",
            "work_for": "中国科学院、水利部成都山地灾害与环境研究所",
            "country": "中国"
        },
        {
            "true_name": "丁海涛",
            "email": "dinghaitao@imde.ac.cn",
            "work_for": "中国科学院、水利部成都山地灾害与环境研究所",
            "country": "中国"
        },
        {
            "true_name": "邓明枫",
            "email": "dmf@imde.ac.cn",
            "work_for": "中国科学院、水利部成都山地灾害与环境研究所",
            "country": "中国"
        }
    ],
    "ds_meta_authors": [
        {
            "true_name": "丁海涛",
            "email": "dinghaitao@imde.ac.cn",
            "work_for": "中国科学院、水利部成都山地灾害与环境研究所",
            "country": "中国"
        }
    ],
    "ds_managers": [
        {
            "true_name": "丁海涛",
            "email": "dinghaitao@imde.ac.cn",
            "work_for": "中国科学院、水利部成都山地灾害与环境研究所",
            "country": "中国"
        },
        {
            "true_name": "陈宁生",
            "email": "chennsh@imde.ac.cn",
            "work_for": "中国科学院、水利部成都山地灾害与环境研究所",
            "country": "中国"
        }
    ],
    "category": "灾害"
}