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Articles 1 - 3 of 3
Full-Text Articles in Physical Sciences and Mathematics
Tb138: Variability Factors Involved With Land Application Of Papermill Sludge, Charles R. Kraske, Ivan J. Fernandez
Tb138: Variability Factors Involved With Land Application Of Papermill Sludge, Charles R. Kraske, Ivan J. Fernandez
Technical Bulletins
The goal of this case study was to assess two components of variability associated with the land application of papermill sludge. These included (1) changes occurring within a temporary sludge stockpile, and (2) spatial variability of application to the site. Understanding the magnitude of such changes will assist in accounting for variability inherent in such land application operations.
Tb137: Chemical And Physical Properties Of The Aurelie, Burnham, Easton, Lille, Linneus, Monadnock, Nicholville, And Tunbridge Soil Map Units, Robert V. Rourke
Tb137: Chemical And Physical Properties Of The Aurelie, Burnham, Easton, Lille, Linneus, Monadnock, Nicholville, And Tunbridge Soil Map Units, Robert V. Rourke
Technical Bulletins
Eight soil map units were sampled at five locations in Maine. The morphology of each site was described and samples were taken from each pedon by horizon for laboratory analyses. Soil samples were analyzed to determine their physical and chemical properties. The data were compiled into composite soil profiles using weighted means. Soil profile descriptions accompanied by the analyses of each pedon sampled are presented.
Soils Of The Ivanhoe Plain, East Kimberley, Western Australia, J M. Aldrick, M H R Van Cuylenburg, P W. Moody, B A. Wren, A J. Clarke
Soils Of The Ivanhoe Plain, East Kimberley, Western Australia, J M. Aldrick, M H R Van Cuylenburg, P W. Moody, B A. Wren, A J. Clarke
Technical Bulletins
The Ivanhoe Plain was divided into two geomorphic provinces. The principal difference between the provinces is the time during which pedogenesis occurred. The crcking clay soils of the northern province are generally more highly leached than their younger counterparts in the southern province. Sixteen land units are identified as distinct from soil units. These units give cognizance to vegetation and topographical features as well as soils.