Matches in SemOpenAlex for { <https://semopenalex.org/work/W3145419110> ?p ?o ?g. }
- W3145419110 endingPage "806" @default.
- W3145419110 startingPage "781" @default.
- W3145419110 abstract "Lavkulich, L. M. and Arocena, J. M. 2011. Luvisols of Canada: Genesis, distribution, and classification. Can. J. Soil Sci. 91: 781–806. Luvisols link the soil continuum on the Quaternary landscapes. These soils are developed from parent materials rich in Ca and Mg in a relatively humid climate. An acidic eluvial horizon overlying a phyllosilicate-enriched illuvial Bt horizon is the common horizon sequence in Luvisolic soils. Lessivage or the translocation of clays with minimal chemical alteration is the characteristic soil-forming process and results to the diagnostic Bt horizon with well-developed, oriented clay skins or cutans. These soils commonly form intergrades with Chernozems, Podzols and Vertisols. With time, the eluvial horizons experience increased chemical weathering and further release of sequioxides to form Brunisolic and Podzolic sequences within the eluvial Ae in biseqeual soils. Lessivage significantly influences several ecosystem functions of soils. The high amounts of phyllosilicates in the Bt horizon serve as one of the most active sorption sites in soils for metals and organic materials including soil carbon. Sorption of cations takes place through cation exchange reactions and determines the availability of cations to plant roots as well as in the “colloid facilitated transport” of strongly sorbing metals and organic pollutants. Clays in Bt can be restrictive to water and air movement as well as to root growth and distribution. Agricultural and forestry practices such as tillage can compact the structure of Luvisols and may decrease soil productivity." @default.
- W3145419110 created "2021-04-13" @default.
- W3145419110 creator A5045557626 @default.
- W3145419110 creator A5070947782 @default.
- W3145419110 date "2011-10-01" @default.
- W3145419110 modified "2023-09-23" @default.
- W3145419110 title "Luvisolic soils of Canada: Genesis, distribution, and classification" @default.
- W3145419110 cites W1542216423 @default.
- W3145419110 cites W1553630333 @default.
- W3145419110 cites W1964897592 @default.
- W3145419110 cites W1967623842 @default.
- W3145419110 cites W1968440806 @default.
- W3145419110 cites W1969007482 @default.
- W3145419110 cites W1971977816 @default.
- W3145419110 cites W1972083510 @default.
- W3145419110 cites W1978133097 @default.
- W3145419110 cites W1978725410 @default.
- W3145419110 cites W1979945185 @default.
- W3145419110 cites W1983285671 @default.
- W3145419110 cites W1985677421 @default.
- W3145419110 cites W1986171098 @default.
- W3145419110 cites W1987281339 @default.
- W3145419110 cites W1988784948 @default.
- W3145419110 cites W1989903373 @default.
- W3145419110 cites W1991011552 @default.
- W3145419110 cites W1991839284 @default.
- W3145419110 cites W1992699997 @default.
- W3145419110 cites W1993164061 @default.
- W3145419110 cites W1995321418 @default.
- W3145419110 cites W1995360580 @default.
- W3145419110 cites W1999602674 @default.
- W3145419110 cites W1999712031 @default.
- W3145419110 cites W2004162342 @default.
- W3145419110 cites W2005463756 @default.
- W3145419110 cites W2008968873 @default.
- W3145419110 cites W2009045485 @default.
- W3145419110 cites W2012692338 @default.
- W3145419110 cites W2015453379 @default.
- W3145419110 cites W2019306900 @default.
- W3145419110 cites W2019931907 @default.
- W3145419110 cites W2019967010 @default.
- W3145419110 cites W2020069211 @default.
- W3145419110 cites W2023104880 @default.
- W3145419110 cites W2027407472 @default.
- W3145419110 cites W2030350494 @default.
- W3145419110 cites W2031703269 @default.
- W3145419110 cites W2032095870 @default.
- W3145419110 cites W2032913072 @default.
- W3145419110 cites W2034742002 @default.
- W3145419110 cites W2035868205 @default.
- W3145419110 cites W2036366045 @default.
- W3145419110 cites W2036653581 @default.
- W3145419110 cites W2037313494 @default.
- W3145419110 cites W2038335935 @default.
- W3145419110 cites W2039338884 @default.
- W3145419110 cites W2042407289 @default.
- W3145419110 cites W2042724877 @default.
- W3145419110 cites W2042910630 @default.
- W3145419110 cites W2043176971 @default.
- W3145419110 cites W2043306356 @default.
- W3145419110 cites W2043646318 @default.
- W3145419110 cites W2043845132 @default.
- W3145419110 cites W2048992058 @default.
- W3145419110 cites W2049193339 @default.
- W3145419110 cites W2049197898 @default.
- W3145419110 cites W2049790053 @default.
- W3145419110 cites W2052390454 @default.
- W3145419110 cites W2054885087 @default.
- W3145419110 cites W2056905750 @default.
- W3145419110 cites W2057436601 @default.
- W3145419110 cites W2059243026 @default.
- W3145419110 cites W2059803473 @default.
- W3145419110 cites W2060280668 @default.
- W3145419110 cites W2060411194 @default.
- W3145419110 cites W2063676435 @default.
- W3145419110 cites W2069445278 @default.
- W3145419110 cites W2070261781 @default.
- W3145419110 cites W2071776973 @default.
- W3145419110 cites W2072140250 @default.
- W3145419110 cites W2074051942 @default.
- W3145419110 cites W2075523039 @default.
- W3145419110 cites W2077009118 @default.
- W3145419110 cites W2078132156 @default.
- W3145419110 cites W2080589461 @default.
- W3145419110 cites W2083072047 @default.
- W3145419110 cites W2083325248 @default.
- W3145419110 cites W2083495260 @default.
- W3145419110 cites W2084496561 @default.
- W3145419110 cites W2085878807 @default.
- W3145419110 cites W2087201655 @default.
- W3145419110 cites W2087678058 @default.
- W3145419110 cites W2092658155 @default.
- W3145419110 cites W2093336772 @default.
- W3145419110 cites W2098830107 @default.
- W3145419110 cites W2099782345 @default.
- W3145419110 cites W2101054218 @default.
- W3145419110 cites W2107795560 @default.
- W3145419110 cites W2109358254 @default.