Titlebook: Digital Soil Morphometrics; Alfred E. Hartemink,Budiman Minasny Book 2016 Springer International Publishing Switzerland 2016 Soil profile

假设

Computer Graphics Procedural Modeling of Soil Structureo-dimensional soil profiles or to generate three-dimensional interactive models that allow rotation, scaling, and other forms of visual explorations. The procedural modeling technique enables the user to generate the soil profile visual representation with only a small amount of data. The images do

Intersect

Soil Profile Imaging for Estimating the Depth Distributions of Clay, Iron, and Hydrological Conditiontly positive correlation was also found between RM and clay content (. = 0.32*, . < 0.05), indicating clay might determine the formation of RM. Moreover, the ratios of iron activity (Fe./Fe.) and iron crystalline ((Fe.-Fe.)/Fe.) could also be good indices for ARD prediction. The Mn./Fe. seemed an i

平常

Variation of Soil Properties in a Mollisol Profile Wallsoil pH demonstrated the lowest horizontal variation in the top 30 cm of the profile. The horizontal variation of Fe concentration tended to increase with depth. Soil property depth functions showed considerable variation between vertical transects. Only the SOC concentration and the soil pH demonst

追踪

Comparative Analysis of Saturated Hydraulic Conductivity (,,) Derived from Image Analysis of Soil Thnt values with field-measured .. and with .. estimated by a PTF using soil texture and bulk density parameters. We digitally scanned 39 thin sections from 11 pedons of soils derived from loess over till and/or over weathered sandstone. Soil voids were classified based on their size and shape. .. was

Carcinogenesis

Measuring and Modelling Soil Depth Functionssitu digital morphometrics by which soil properties are measured along a soil profile wall at small depth increments. We explore the possibility of horizon boundary detection based on the changes in elemental concentrations. It was concluded that digital morphometrics enables soil scientists to meas

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