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青藏高原高寒荒漠区土壤湿度监测仪器的校正方法探讨 被引量:3
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作者 谢芳荻 阎建忠 +4 位作者 刘林山 张镱锂 王兆锋 李兰晖 李彩瑛 《地理研究》 CSSCI CSCD 北大核心 2017年第11期2112-2128,共17页
ECH_2O EC-5土壤水分传感器能有效地监测土壤含水量,并且能揭示不同降水事件下的土壤水分动态变化状况。然而青藏高原主要土壤类型砾石含量高、昼夜温差大、秋季和春季冻融现象显著,导致监测数据出现偏差。基于对羌塘高原日土、改则地... ECH_2O EC-5土壤水分传感器能有效地监测土壤含水量,并且能揭示不同降水事件下的土壤水分动态变化状况。然而青藏高原主要土壤类型砾石含量高、昼夜温差大、秋季和春季冻融现象显著,导致监测数据出现偏差。基于对羌塘高原日土、改则地区布设的野外观测站点采集的土壤样品,对其进行土壤含水量测定的室内标定试验。结果表明:(1)各个样点均获得了较好的拟合效果,基于拟合系数校正后的测量值可以有效地反映实际的土壤含水量情况;(2)不同土层深度及不同样点的综合校准曲线精度明显低于单点的校准结果,主要受土壤容重和有机碳含量的影响,为获取更精准的校正数据,分层的校准是很有必要的;(3)基于已有校准模型校正后的值可以反映含水量变化的整体态势,但会产生高估或低估于真实值的偏离。 展开更多
关键词 土壤体积含水量 校正 介电常数 容重 温度 青藏高原
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1990-2015年喜马拉雅山脉中段柯西河流域土地覆被垂直带变化
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作者 吴雪 PAUDEL Basanta +5 位作者 张镱锂 刘林山 王兆锋 谢芳荻 高俊刚 孙晓敏 《Journal of Geographical Sciences》 SCIE CSCD 2021年第10期1419-1436,共18页
The study of mountain vertical natural belts is an important component in the study of regional differentiation.These areas are especially sensitive to climate change and have indicative function,which is the core of ... The study of mountain vertical natural belts is an important component in the study of regional differentiation.These areas are especially sensitive to climate change and have indicative function,which is the core of three-dimensional zonality research.Thus,based on high precision land cover and digital elevation model(DEM)data,and supported by MATLAB and ArcGIS analyses,this paper aimed to study the present situation and changes of the land cover vertical belts between 1990 and 2015 on the northern and southern slopes of the Koshi River Basin(KRB).Results showed that the vertical belts on both slopes were markedly different from one another.The vertical belts on the southern slope were mainly dominated by cropland,forest,bare land,and glacier and snow cover.In contrast,grassland,bare land,sparse vegetation,glacier and snow cover dominated the northern slope.Study found that the main vertical belts across the KRB within this region have not changed substantially over the past 25 years.In contrast,on the southern slope,the upper limits of cropland and bare land have moved to higher elevation,while the lower limits of forest and glacier and snow cover have moved to higher elevation.The upper limit of alpine grassland on the northern slope retreated and moved to higher elevation,while the lower limits of glacier and snow cover and vegetation moved northward to higher elevations.Changes in the vertical belt were influenced by climate change and human activities over time.Cropland was mainly controlled by human activities and climate warming,and the reduced precipitation also led to the abandonment of cropland,at least to a certain extent.Changes in grassland and forest ecosystems were predominantly influenced by both human activities and climate change.At the same time,glacier and snow cover far away from human activities was also mainly influenced by climate warming. 展开更多
关键词 vertical belt land cover Central Himalayas Koshi River Basin climate change
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