2005
DOI: 10.1016/j.foreco.2004.09.009
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Soil chemistry and nutrient regimes following 17–21 years of shortleaf pine-bluestem restoration in the Ouachita Mountains of Arkansas

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Cited by 15 publications
(11 citation statements)
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“…Positive correlation between these two variables has been reported by several authors (Beery and Wilding, 1971;Caires et al, 2006;Liechty et al, 2005). It is expected, with the increase in soil pH, that Al 3+ precipitates, CEC increases and exchange sites be occupied by Ca 2 + and Mg 2+ released from lime or organic fertilizer (Martins et al, 2014;Matschonat and Falkengren-Grerup, 2000).…”
Section: Base Saturationmentioning
confidence: 52%
“…Positive correlation between these two variables has been reported by several authors (Beery and Wilding, 1971;Caires et al, 2006;Liechty et al, 2005). It is expected, with the increase in soil pH, that Al 3+ precipitates, CEC increases and exchange sites be occupied by Ca 2 + and Mg 2+ released from lime or organic fertilizer (Martins et al, 2014;Matschonat and Falkengren-Grerup, 2000).…”
Section: Base Saturationmentioning
confidence: 52%
“…Shortleaf pine is currently the focus of a major restoration effort (Shortleaf Pine Initiative: http://shortleafpine.net/) throughout its native range [20,21] because of the suite of ecosystem services they provide. Shortleaf pine restoration leads to increased levels of plant available nutrients over time [22], in spite of initial loss of nitrogen [23]. Shortleaf pine restoration also provides important habitat for the federally endangered red-cockaded woodpecker (Picoides borealis), and also positively impacts diversity and/or abundance of populations of taxa including butterflies, reptiles, amphibians [24], other birds [25,26] and small mammals [27].…”
Section: Shortleaf Pine Restorationmentioning
confidence: 99%
“…Fire can lead to important changes in the physical and chemical properties of forest soils including increased bulk density and altered physical structure (Boyer and Miller, 1994;Arocena and Opio, 2003), increased soil cation stocks (Franklin et al, 2003;Liechty et al, 2005;Neff et al, 2005), and decreased carbon (C) and nitrogen (N) stocks in surface soils (Binkley, 1992;Choromanska and DeLuca 2001;MacKenzie et al, 2004;Shelburne et al, 2004). Responses of soil cations, C and N to fire vary substantially in direction, magnitude and the length of time during which changes can be detected after fire (Carter and Foster, 2004;Certini, 2005).…”
Section: Introductionmentioning
confidence: 99%