Zobrazeno 1 - 10
of 282
pro vyhledávání: '"R G Kachanoski"'
Publikováno v:
Water Resources Research. 36:3767-3767
Publikováno v:
Canadian Journal of Soil Science. 93:173-191
Woods, S. A., Dyck, M. F. and Kachanoski, R. G. 2013. Spatial and temporal variability of soil horizons and long-term solute transport under semi-arid conditions. Can. J. Soil Sci. 93: 173–191. Characterizing the spatial and temporal variability of
Autor:
Miles Dyck, R. G. Kachanoski
Publikováno v:
Canadian Journal of Soil Science. 91:149-159
Dyck, M. F. and Kachanoski, R. G. 2011. Scale-dependent covariance of soil physical properties above and below a soil horizon interface: Pedogenic versus anthropogenic influences on total porosity. Can. J. Soil Sci. 91: 149–159. The basic unit of s
Autor:
R. G. Kachanoski, Miles Dyck
Publikováno v:
Vadose Zone Journal. 9:385-396
Preferential flow at the Darcian scale may manifest as a consistent spatial pattern of high- and low-flow domains. The degree of persistence of these high- and low-flow domains with depth has important implications for the prediction of subsurface co
Autor:
R G Kachanoski
Publikováno v:
Canadian Journal of Soil Science. 89:543-554
Estimation of fertilizer N requirements of crops remains a challenge. Numerous field studies have been carried out to calibrate soil tests against yield response to applied fertilizer N. Synthesis and identification of common crop fertilizer N respon
Autor:
M. F. Dyck, R. G. Kachanoski
Publikováno v:
Soil Science Society of America Journal. 73:1786-1795
Soil horizon interfaces have been shown to be focal points for localized, three-dimensional redistribution of water and solutes in field soils. Therefore, understanding of the physics of water flow and transport in layered soils requires experimental
Autor:
R. G. Kachanoski, Miles Dyck
Publikováno v:
Soil Science Society of America Journal. 73:1604-1613
Understanding the physics oF water flow and transport in layered soils requires experimental observations of the magnitude and variability of these processes as they occur in the field. In this study, a time domain reflectometry (TDR) method to measu
Publikováno v:
Proceedings of the Fourth International Conference on Precision Agriculture
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9b7aeaa17ecd2be8b65fd28605e2a881
https://doi.org/10.2134/1999.precisionagproc4.c30
https://doi.org/10.2134/1999.precisionagproc4.c30
Publikováno v:
Vadose Zone Journal. 4:915-923
Knowledge about the magnitude and variability of water and solute fluxes in semiarid environments is required to assess the environmental risk associated with contaminants in the vadose zone. The purpose of this study was to examine the pedon-scale s
Autor:
R. G. Kachanoski, C. J. Hamlen
Publikováno v:
Soil Science Society of America Journal. 68:404-416
The effect of initial soil water content (0) and steady and transient water flow boundary conditions (J w ) on the transport of identical solute pulses was examined in four undisturbed soil columns. Solute breakthrough curves (BTCs) and 0 were monito