石河子大学学报(自然科学版)
石河子大學學報(自然科學版)
석하자대학학보(자연과학판)
JOURNAL OF SHIHEZI UNIVERSITY (NATURAL SCIENCE)
2014年
1期
79-85
,共7页
徐璐%李平衡%赵鑫%杨广%何新林
徐璐%李平衡%趙鑫%楊廣%何新林
서로%리평형%조흠%양엄%하신림
荒漠植物%液流%日变化%环境因子%尺度上推
荒漠植物%液流%日變化%環境因子%呎度上推
황막식물%액류%일변화%배경인자%척도상추
desert plants%sap flow%diurnal change%environment factors%up-scaling
针对西北干旱荒漠区水分循环与生态平衡问题,利用热扩散(TDP)探针监测典型荒漠植物梭梭和柽柳的枝条和胸径的液流日变化,并分析不同尺度液流与环境因子的关系及其尺度间的转换方法。结果表明:梭梭和柽柳的枝条和胸径的液流开始时间基本与太阳辐射开始增强的时间一致,且都滞后于温度和水气压亏缺(VPD)的开始升高时间。太阳总辐射是植物液流的启动器,而VPD是植物液流的加速器。不同环境因子对梭梭和柽柳不同尺度液流的影响作用不同,整体相关性大小为:总辐射>光合有效辐射>温度>VPD。梭梭枝条间差异不明显,可以较好的上推出胸径的液流密度,即梭梭枝条尺度和冠层尺度间蒸腾作用可以较好的转换:y=1.925x+0.569,R2=0.956。柽柳枝条间差异较大,枝条液流与胸径液流间的相关性相对较小(y=2.418x+0.808,R2=0.697),把枝条液流上推到胸径尺度需分析不同位置的枝条间液流的差异性及其与微环境的关系,进一步修正尺度上推方程。
針對西北榦旱荒漠區水分循環與生態平衡問題,利用熱擴散(TDP)探針鑑測典型荒漠植物梭梭和檉柳的枝條和胸徑的液流日變化,併分析不同呎度液流與環境因子的關繫及其呎度間的轉換方法。結果錶明:梭梭和檉柳的枝條和胸徑的液流開始時間基本與太暘輻射開始增彊的時間一緻,且都滯後于溫度和水氣壓虧缺(VPD)的開始升高時間。太暘總輻射是植物液流的啟動器,而VPD是植物液流的加速器。不同環境因子對梭梭和檉柳不同呎度液流的影響作用不同,整體相關性大小為:總輻射>光閤有效輻射>溫度>VPD。梭梭枝條間差異不明顯,可以較好的上推齣胸徑的液流密度,即梭梭枝條呎度和冠層呎度間蒸騰作用可以較好的轉換:y=1.925x+0.569,R2=0.956。檉柳枝條間差異較大,枝條液流與胸徑液流間的相關性相對較小(y=2.418x+0.808,R2=0.697),把枝條液流上推到胸徑呎度需分析不同位置的枝條間液流的差異性及其與微環境的關繫,進一步脩正呎度上推方程。
침대서북간한황막구수분순배여생태평형문제,이용열확산(TDP)탐침감측전형황막식물사사화정류적지조화흉경적액류일변화,병분석불동척도액류여배경인자적관계급기척도간적전환방법。결과표명:사사화정류적지조화흉경적액류개시시간기본여태양복사개시증강적시간일치,차도체후우온도화수기압우결(VPD)적개시승고시간。태양총복사시식물액류적계동기,이VPD시식물액류적가속기。불동배경인자대사사화정류불동척도액류적영향작용불동,정체상관성대소위:총복사>광합유효복사>온도>VPD。사사지조간차이불명현,가이교호적상추출흉경적액류밀도,즉사사지조척도화관층척도간증등작용가이교호적전환:y=1.925x+0.569,R2=0.956。정류지조간차이교대,지조액류여흉경액류간적상관성상대교소(y=2.418x+0.808,R2=0.697),파지조액류상추도흉경척도수분석불동위치적지조간액류적차이성급기여미배경적관계,진일보수정척도상추방정。
Aiming at solving the problem of hydrological cycle and ecological balance in northwest arid desert,thermal dissipation probes (TDP) were used to monitor diurnal change characteristic of sap flow in two desert plants Haloxylon ammodendron and Tamarix chinensis in branch and canopy scales,respectively.The relationships of sap flow in different scales and environment factors,as well as up-scaling were analyzed.The results showed that the two plants sap flow start time in both scales (branch scale and canopy scale) were basically in accordance with the time of solar radiance beginning to enhance,and lagged behind the time of temperature and VPD (vapour pressure deficit) beginning to rise.Global radiance was the launcher of plant sap flow,while VPD was the accelerator.The different environment factors influenced dissimilarly on sap flow of two plants in different scales,and the correlations between environment factors and sap flow were global radiance >photosynthetically active radiation (PAR) > temperature > VPD.Sap flows of Haloxylon ammodendron branches which had no significant difference could be used to upscale the sap flow of the DBH.That was to say, the transpiration of Haloxylon ammodendron in different scales could transform well:y=1.925x+0.569,R2=0.956.While sap flows of Tamarix chinensis branches which had difference could not be used very well to upscale the sap flow of the DBH:y=2.418x+0.808,R2=0.697.Transpiration up-scaling from branch to canopy needed to analyse the different R2 of sap flow of branches in different positions and the relationship with microenvironment,and modified the up-scaling formula further.