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Mineral Soil Chemical Properties as Influenced by Long-Term Use of Prescribed Fire with Differing Frequencies in a Southeastern Coastal Plain Pine Forest

机译:矿物土壤化学性质受到在东南沿海普遍林林森林中长期使用规定火灾的规定火灾的影响

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摘要

Recent studies suggest increased fire frequency may impair soil chemistry, but few studies have examined long-term effects of repeated, frequent prescribed fires on forest soil properties in the southeastern Coastal Plain, USA. In this study, forest soil chemistry at the 0⁻10 and 10⁻20 cm mineral soil depths of sandy surface horizons (Entisols and Spodosols) were compared among units burned 0, 4, 6, and 8 times between 2004 and 2015 and 0 and 20 times between 1978 and 2015 in a longleaf (Pinus palustris Mill.)⁻loblolly (Pinus taeda L.) pine savanna at the Tom Yawkey Wildlife Center (Georgetown, SC, USA). At the 0⁻10 cm soil depth, soil pH (p = 0.00), sulfur (p = 0.01), calcium (p = 0.01), iron (p < 0.01), manganese (p < 0.01), and aluminum (p = 0.02) treatment means differed (2004⁻2015). Calcium and manganese displayed positive, significant relationships and sulfur displayed a negative, significant relationship with increasing fire frequency (p < 0.05). However, correlation of these relationships was low (r2 ≤ 0.23). Using linear contrasts to compare the mean of all fire treatments (20 fires from 1978 to 2015) to the mean of the unburned compartment, sulfur (p = 0.01) and iron (p < 0.01) were less in soils from the burned compartments. At the 10⁻20 cm soil depth, soil pH (p = 0.01), manganese (p = 0.04), phosphorus (p = 0.01), potassium (p = 0.02), and iron (p < 0.01) treatment means differed (2004⁻2015). Potassium displayed a negative, significant relationship and soil pH displayed a positive, significant relationship with increasing fire frequency (p < 0.05). Correlation of these relationships was low (r2 ≤ 0.16), however. Using linear contrasts to compare the mean of all fire treatments (20 fires from 1978 to 2015) to the unburned compartment, potassium (p = 0.00) and iron (p < 0.01) were less in soils from burned compartments. These results are inconsistent with studies suggesting that forest soil chemistry is substantially altered by increased fire frequency and support other studies from this region that have documented minimal or temporary soil chemical changes associated with frequent prescribed fires.
机译:最近的研究表明增加了火灾的频率可能会影响土壤的化学成分,但很少有研究探讨在东南沿海平原,森林美国土壤性质重复的,频繁的规定火灾的长期影响。在这项研究中,在砂质地面视野的0⁻10和10⁻20厘米矿土深度(新成土和灰土)森林土壤化学单元之间进行比较2004和2015和0之间烧0,4,6,和8倍在长叶1978年和2015年间的20倍(长叶松磨。)⁻loblolly(火炬松)松稀树草原在汤姆·亚基野生动物中心(乔治城,SC,USA)。在0⁻10厘米土壤深度,土壤的pH值(P = 0.00),硫(P = 0.01),钙(P = 0.01),铁(P <0.01),锰(P <0.01)和铝(p值= 0.02)治疗手段不同(2004⁻2015)。钙和锰显示阳性,显著关系和硫显示负,显著关系随着火频率(P <0.05)。然而,这些关系的相关性较低(R2≤0.23)。使用线性对比于平均的所有火处理(20起火灾1978年至2015年)比较平均的未燃室,硫(P = 0.01)和铁(P <0.01)不太在土壤中从燃烧室。差异在10⁻20厘米土壤深度,土壤pH值(P = 0.01),锰(P = 0.04),磷(P = 0.01),钾(P = 0.02),和铁(P <0.01)处理装置(2004年⁻2015)。钾显示负,显著关系和土壤pH值显示随着火频率(P <0.05)的正,显著的关系。这些关系的相关性较低(R2≤0.16),但是。使用线性对比于平均的所有火处理(20起火灾1978至2015年)比较的未燃室,钾(P = 0.00)和铁(P <0.01)在从燃烧室的土壤是以下。这些结果与研究表明森林土壤化学基本被增加了火灾的频率改变,并从该地区已记录频繁规定的火灾相关的微量或临时土壤的化学变化支持其他研究不一致。

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