26 research outputs found
Deficiencies in the soil quality concept and its application
Soil quality is a concept that has deeply divided the soil science community. It has
been institutionalized and advocated without full consideration of concept weaknesses and
contradictions. Our paper highlights its disfunctional definition, flawed approach to
quantification, and failure to integrate simultaneous functions, which often require contradictory
soil properties and/or management. While the concept arose from a call to protect the
environment and sustain the soil resource, soil quality indexing as implemented may actually
impair some soil functions, environmental quality, or other societal priorities. We offer the
alternative view that emphasis on known principles of soil management is a better expenditure of
limited resources for soil stewardship than developing and deploying subjective indices which fail
to integrate across the necessary spectrum of management outcomes. If the soil quality concept
is retained, we suggest precisely specifying soil use, not function or capacity, as the criteria for
attribute evaluation. Emphasis should be directed toward using available technical information to
motivate and educate farmers on management practices that optimize the combined goals of high
crop production, low environmental degradation, and a sustained resource
Tamanho de amostras para a determinação de parâmetros físicos em planossolo por tomografia computadorizada
A técnica da tomografia computadorizada (TC) permite medir a densidade e a umidade de amostras de solo, constituindo uma importante ferramenta na Ciência do Solo. Este trabalho tem como objetivos descrever os aspectos da adequação do tamanho de amostras de um Planossolo e os procedimentos de avaliação e estudos por análise estatística, empregando-se um minitomógrafo computadorizado de raios gama com fonte de 241Am. O valor do erro atribuído ao equipamento são 0,051 e 0,046 Mg m-3, respectivamente, para os horizontes A e B. O valor teórico da espessura da amostra do Planossolo para uso na técnica de TC com fonte de 241Am é, aproximadamente, 4,0 cm para os horizontes A e B. Já a espessura ideal de amostras é de aproximadamente 6,0 cm, sendo menor para amostras do horizonte B em relação ao A. Obteve-se boa precisão e adaptabilidade no emprego da TC para estudos de Planossolos._________________________________________________________________________________ ABSTRACT: Computerized tomography (CT) is an important tool in Soil Science for noninvasive measurement of density and water content of soil samples. This work aims to describe the aspects of sample size adequacy for Planosol (Albaqualf) and to evaluate procedures for statistical analysis, using a CT scanner with a 241Am source. Density errors attributed to the equipment are 0.051 and 0.046 Mg m-3 for horizons A and B, respectively. The theoretical value for sample thickness for the Planosol, using this equipment, is 4.0 cm for the horizons A and B. The ideal thickness of samples is approximately 6.0 cm, being smaller for samples of the horizon B in relation to A. Alternatives for the improvement of the efficiency analysis and the reliability of the results obtained by CT are also discussed, and indicate good precision and adaptability of the application of this technology in Planosol (Albaqualf) studies
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Helical Pulse Line Structures for Ion Acceleration
The basic concept of the ''Pulse Line Ion Accelerator'' is presented, where pulse power sources create a ramped traveling wave voltage pulse on a helical pulse line. Ions can surf on this traveling wave and achieve energy gains much larger than the peak applied voltage. Tapered and untapered lines are compared, and a transformer coupling technique for launching the wave is described
Deficiencies in the soil quality concept and its application
Soil quality is a concept that has deeply divided the soil science community. It has
been institutionalized and advocated without full consideration of concept weaknesses and
contradictions. Our paper highlights its disfunctional definition, flawed approach to
quantification, and failure to integrate simultaneous functions, which often require contradictory
soil properties and/or management. While the concept arose from a call to protect the
environment and sustain the soil resource, soil quality indexing as implemented may actually
impair some soil functions, environmental quality, or other societal priorities. We offer the
alternative view that emphasis on known principles of soil management is a better expenditure of
limited resources for soil stewardship than developing and deploying subjective indices which fail
to integrate across the necessary spectrum of management outcomes. If the soil quality concept
is retained, we suggest precisely specifying soil use, not function or capacity, as the criteria for
attribute evaluation. Emphasis should be directed toward using available technical information to
motivate and educate farmers on management practices that optimize the combined goals of high
crop production, low environmental degradation, and a sustained resource
Recommended from our members
Overview of The Pulse Line Ion Accelerator
An overview of the Pulse Line Ion Accelerator (PLIA) concept and its development is presented. In the PLIA concept a pulse power driver applied to one end of a helical pulse line creates a traveling wave pulse that accelerates and axially confines a heavy ion beam pulse The motivation for its development at the IFE-VNL is the acceleration of intense, short pulse, heavy ion beams to regimes of interest for studies of High Energy Density Physics and Warm Dense Matter. Acceleration scenarios with constant parameter helical lines are described which result in output energies of a single stage much larger than the several hundred kilovolt peak voltages on the line, with a goal of 3-5 MeV/meter acceleration gradients. The main attraction of the concept is the very low cost it promises. It might be described crudely as an ''air core'' induction linac where the pulse-forming network is integrated into the beam line so the accelerating voltage pulse can move along with the ions to get voltage multiplication