实测高光谱和HSI影像的区域土壤盐渍化遥感监测研究

通过典型研究区不同盐渍化土壤光谱反射率数据的变换和分析,选择与土壤含盐量响应敏感波段,建立实测高光谱土壤含盐量反演模型,以校正HSI影像建立的土壤含盐量反演模型。结果表明：实测高光谱土壤含盐量反演模型与HSI影像土壤含盐量反演模型均有较好的精度,模型判定系数(R2)均高于0.57,且模型稳定性较好。校正后的HSI影像土壤含盐量反演模型,模型判定系数有了较大提高,R2从0.571提升至0.681,且通过了0.01的显著性水平,均方根误差(RMSE)值为0.277。模型能够较好地提高区域尺度条件下土壤盐渍化监测精度,运用此方法开展盐渍化土壤定量遥感监测是可行的。     

基于实测高光谱和电磁感应数据的区域土壤盐渍化遥感监测研究

以新疆渭干河—库车河三角洲绿洲为例,利用实测得到的不同盐渍化程度的盐渍土高光谱数据和电磁感应数据(EM38)协同构建土壤高光谱盐分指数遥感监测模型,将该模型通过尺度效应转换用于校正传统的Landsat-TM多光谱遥感影像的土壤盐分光谱指数,用校正过的TM影像进行区域土壤盐分的反演,并利用实测土壤盐分数据对反演结果进行分析与验证。结果表明：将高光谱和电磁感应数据与多光谱遥感技术相结合进行区域土壤盐渍化信息的提取,其精度和反演效果(R2=0.799 3,p<0.01)明显优于传统多光谱遥感方法中单纯利用土壤盐分指数所建立的监测模型(R2=0.587 4,p<0.01),为今后更好地实现土壤盐渍化的高精度遥感动态监测研究提供了科学依据。     

Fisher–KPP equation on the Heisenberg group

In this paper, we consider the Fisher–KPP equation on the Heisenberg group. We discuss the existence of global solutions, asymptotic behavior of global solutions and blow-up solutions. Moreover, we extend the obtained results to the time-fractional Fisher–KPP equation on the Heisenberg group.     

Layered Intergrowth Phases Bi4MO8X (X=Cl, M=Ta and X=Br, M=Ta or Nb): Structural and Electrophysical Characterization

The high-temperature structural behavior of the layered intergrowth phase Bi₄TaO₈Cl, belonging to the Sillén-Aurivillius family, has been studied by powder neutron diffraction. This material is ferroelectric, space group P2₁cn, at T_C<640 K. An order-disorder transition to centrosymmetric space group Pmcn is found around 640 K, which involves disordering of TaO₆ octahedral tilts. A second phase transition, of a first-order nature, to space group P4/mmm occurs at a temperature of ∼1038 K. The crystal structures of the bromide analogs Bi₄MO₈Br (M=Nb, Ta) have also been determined at room temperature; both are isomorphous with Bi₄TaO₈Cl and exhibit maxima in dielectric constant at temperatures of approximately 588 and 450 K, respectively.