2004
DOI: 10.1016/j.still.2002.12.001
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Temporal variation of soil compaction and deterioration of soil quality in pasture areas of Colombian Amazonia

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Cited by 185 publications
(137 citation statements)
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“…Soil compaction Although a number of studies from tropical countries have demonstrated advantages of adopting more intensive pasture management, it may lead to increased soil compaction from trampling and ultimately to productivity losses, if management is not performed correctly (Martinez and Zinck, 2004). Compaction of the topsoil resulting from the pressure exerted by the hooves of an increased number of cattle per unit area has been shown to negatively impact soil physical conditions: increasing bulk density and penetration resistance, decreasing soil porosity and infiltration rates.…”
Section: Factors Related To Sustainability Of Intensificationmentioning
confidence: 99%
“…Soil compaction Although a number of studies from tropical countries have demonstrated advantages of adopting more intensive pasture management, it may lead to increased soil compaction from trampling and ultimately to productivity losses, if management is not performed correctly (Martinez and Zinck, 2004). Compaction of the topsoil resulting from the pressure exerted by the hooves of an increased number of cattle per unit area has been shown to negatively impact soil physical conditions: increasing bulk density and penetration resistance, decreasing soil porosity and infiltration rates.…”
Section: Factors Related To Sustainability Of Intensificationmentioning
confidence: 99%
“…The effect of trampling by cattle on microbial community is less studied. In tropical forest Martinez and Zinck (2004) showed evidence of soil compaction through cattle trampling after clearing primary forests. Compaction implies an increase in soil bulk density and in soil strength and consequently a decrease in air permeability and hydraulic conductivity (Whalley et al, 1995).…”
Section: Introductionmentioning
confidence: 99%
“…Das durchschnittliche C:N-Verhältnis schwankte im Oberboden zwischen 9,6 und 11,1 und im Unterboden zwischen 10,3 und 11,6 (Tabelle 2 (Vepraskas, 1988;Martinez und Zinck, 2004). Allerdings wird mit steigendem Bodenwassergehalt der Zusammenhang zwischen EW und LD zunehmend schwächer (Vaz et al, 2001), weil der Boden plastischer wird.…”
Section: Bodenart Und Bodenchemische Kennwerteunclassified