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Determination of Anisotropy of Tills by Means of Azimuthal Resistivity and Conductivity Measurements
Determination of Anisotropy Means of Azimuthal Resistivity Conductivity Measurements
2009/10/23
Anisotropy of glacial tills in Lapland revealed with azimuthal galvanic (Terrameter 300 C) resistivity and inductive (Geonics EM-31) electrical conductivity measurements, which were carried out at fou...
Retrieval of canopy component temperatures through Bayesian inversion of directional thermal measurements
temperatures thermal measurements
2009/7/22
Evapotranspiration is usually estimated in remote sensing from single temperature value representing both soil and vegetation. This surface temperature is an aggregate over multiple canopy components...
Plot Measurements of Snowmelt Runoff for Varying Soil Conditions
Plot Measurements Snowmelt Runoff Varying Soil Conditions
2009/6/15
Plot Measurements of Snowmelt Runoff for Varying Soil Conditions.
A comparison between reference transpiration and measurements of evaporation for a riparian grassland site
transpiration evaporation riparian grassland site
2009/5/27
This paper compares direct measurements of evaporation with the values predicted for reference transpiration. The measurements of actual evaporation were made using an eddy correlation device on a gra...
Determination of fluid transmissivity and electric transverse resistance for shallow aquifers and deep reservoirs from surface and well-log electric measurements
Fluid transmissivity time resistivity times permeability fluid potential
2009/5/26
Fluid transmissivity (layer thickness times permeability) and electric transverse resistance (layer thickness time resistivity) are important parameter in groundwater and hydrocarbon exploration. Dete...
Characterization of spatial heterogeneity of groundwater-stream water interactions using multiple depth streambed temperature measurements at the reach scale
water fluxes heat conduction-advection streambed temperature
2009/5/15
Streambed temperatures can be easily, accurately and inexpensively measured at many locations. To characterize patterns of groundwater-stream water interaction with a high spatial resolution, we measu...