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After various considerations, we decided to only use soil profile observations which have clear geographical coordinates.
We determined mean residence time (MRT) and peak marker concentration using the original profile observations and regressions.
We designed a database for soil profile observations and implemented it at two levels: spatial site data and horizon data.
The surface profile observations provided information of a small contribution of grain boundary sliding to the creep process when grain boundaries are not closely perpendicular to the stress.
In this study, a national soil map of Denmark was constructed based on the FAO–Unesco Revised Legend 1990 using digital soil mapping techniques, existing soil profile observations and environmental data.
To develop a capable ensemble-based scheme for operationally assimilating Argo profile observations into a hybrid coordinate ocean model (HYCOM), we compared some different ensemble optimal interpolation (EnOI) schemes, which can be divided into two different kinds.
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This refers to soil profile observation and description data, laboratory and field analytical data, and also derived products such as digital soil maps and soil property estimations, and interpreted information based on agreed and representative indicator sets.
For the jth sample collected over time, the observations are denoted by (x i, y ij ), i = 1, 2, …, n, where it is assumed there exist an auto-correlation between the error terms and that within-profile observations at different values of the predictor variable x are modeled by a first-order auto-regressive, AR(1), model.
We evaluated the GEOS-Chem simulation of the aerosol vertical profile using observations from the Cloud-Aerosol LIDAR and Infrared Pathfinder Satellite Observation (CALIPSO) satellite (Winkler et al. 2007).
To determine whether a structure in the image was a nerve-fiber profile, simultaneous observations of the image on a high-resolution computer monitor and the section viewed in the microscope were performed.
In order to monitor the surface movement and deformation characteristics, surface movement observation stations were established by adopt the layout method of profile striation observation station according to the situation of landform and terrain and the mining geological conditions in the SLW face (Zou et al. 2003).
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