{"id":"2c8cc4cf-cd78-4ae1-b5f0-f24a6a85ac30","title":"黑河排露沟流域海拔2800m青海云杉林林地蒸量数据集（2011-2013）","title_en":"Soil evaporation dataset of Qinghai spruce stand at 2800m above sea level in Pailougou watershed (2011-2013)","serial":"黑河计划","user_limit":"本数据由“黑河流域上游青海云杉林蒸散特征及其耗水机制研究”项目产生，用户在使用数据时请在正文中明确声明数据的来源，并在参考文献部分引用本元数据提供的引用方式","instructions":"excel 格式存储","description":"林地土壤蒸发是土壤中的水分通过上升和汽化从土壤表面进入大气的过程。土壤蒸发影响土壤含水量的变化，是水文循环的一个重要环节。该数据通过自制的minilysmeter蒸发筒观测的，目的是为研究青海云杉林水分垂向交换规律提供数据支撑。","doi":"10.3972/heihe.004.2014.db","projection":null,"language":"zh","share_type":"offline","east":100.307,"west":100.286,"south":38.529,"north":38.558,"scale":null,"crs":null,"filesize":0.1,"share_policy":"c","ts_created":"2014-04-30T17:46:05+08:00","doi_type":"","ts_updated":"2021-04-19T23:25:36.347392+08:00","time_description":"","datas_group":0,"time_description_en":"","data_format":"EXCEL","project":[10,11,15],"specials":["4e7b97a6-ee1f-4b51-83e5-04a100993973"],"cite":"常学向, 黑河排露沟流域海拔2800m2011-2013年青海云杉林林地蒸量数据集，黑河计划数据管理中心, 2014. doi:10.3972/heihe.004.2014.db","review_status":5,"review_invite":[],"review_editor":null,"data_sources":null,"temporal_resolution":null,"spatial_resolution":null,"license":"Attribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-SA 4.0)","fund":[145],"subtopics":{"metadata":"2c8cc4cf-cd78-4ae1-b5f0-f24a6a85ac30","three_pole":null,"third_pole":null},"username":"常学向","review_time":null,"protected_duration":6,"protected_describe":null,"is_important":false,"hit_count":8672}