2007
DOI: 10.1016/j.foreco.2007.01.023
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Long-term influence of site preparation on water-retention characteristics of forest soil in Finnish Lapland

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Cited by 13 publications
(16 citation statements)
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“…The amount of moisture retained at a given tension increases with decreasing particle size and with increasing organic matter content (Wesseling et al, 2009b). It therefore varies with soil type (Batjes, 1996), land use (Heiskanen et al, 2007;Bormann and Klaassen, 2008), management (Ahuja et al, 1998;Katsvairo et al, 2002) and topographical position (Pachepsky et al, 2001). The soil water retention characteristics largely determine the amount of water available for plant growth.…”
Section: Introductionmentioning
confidence: 99%
“…The amount of moisture retained at a given tension increases with decreasing particle size and with increasing organic matter content (Wesseling et al, 2009b). It therefore varies with soil type (Batjes, 1996), land use (Heiskanen et al, 2007;Bormann and Klaassen, 2008), management (Ahuja et al, 1998;Katsvairo et al, 2002) and topographical position (Pachepsky et al, 2001). The soil water retention characteristics largely determine the amount of water available for plant growth.…”
Section: Introductionmentioning
confidence: 99%
“…The determination of soil organic matter content, bulk density (BD), particle density (PD) and water content (WC) at c (0.3, (1, (5, (10, (100 and (1500 kPa in the laboratory have earlier been described in detail (Heiskanen and Ma¨kitalo 2002). The water retention at c 0 kPa was also estimated on the basis of the total porosity, which was calculated as [(PD Á BD)/PD], and added to six measured WC values (Heiskanen et al 2007;Al Majou et al 2008).…”
Section: Soil Physical Propertiesmentioning
confidence: 99%
“…It has earlier been shown that site preparation does not alter SWC (Mannerkoski and Mo¨tto¨nen 1990;Ma¨kitalo and Hyvo¨nen 2004;Ma¨kitalo et al 2006) nor water retention characteristics, including the van Genuchten model parameters (Heiskanen et al 2007) in the intact intermediate areas. Consequently, it can be concluded that the soil physical properties in intermediate areas represent the ''original site properties'' before clearcutting and site preparation.…”
mentioning
confidence: 97%
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“…Allelopathic effects in the ground layer of vegetation also may limit seed germination and seedling growth [17,18]. MSP can modify the physical properties of soil, such as water content, aeration, temperature and bulk density, as well as its chemical properties, such as organic matter content, nutrient availability and pH [19][20][21][22]. Furthermore, most site preparation methods can cause soil erosion if not carefully implemented and adapted to the specific site characteristics and climate [23,24].…”
Section: Introductionmentioning
confidence: 99%