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Fire exclusion and nitrogen mineralization in low elevation forests of western Montana.

机译:蒙大拿州西部低海拔森林的防火和氮矿化作用。

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Little is known regarding how fire exclusion influences nitrogen (N) cycling in low elevation forests of western Montana. Nor is it clear how the change in fire frequency that has resulted from forest management has influenced ecosystem function in terms of plant-soil-microbe interactions. A fire chronosequence approach was used to examine the influence of forest succession on soil biochemical properties and microbimal activity at 10 sites with varying time since fire (2-130 years). The rate of decomposition of buried tongue depressors and cotton strips, was found to decrease significantly (R2=0.410, P=0.087 and R2=0.761, P=0.003, respectively) with time since fire (TSF). Net N mineralization and nitrification, as estimated by resin sorbed NH4+ and NO3- concentrations, both exhibited significant non-linear decreases (R2=0.870, P=0.000 and R2=0.620, P=0.007, respectively) with TSF. Nitrification potential measured using an aerated soil slurry method, also decreased significantly (R2=0.595, P=0.009) with TSF. These decreases in N availability along with an increase in the metabolic quotient and a decrease in labile C pools with TSF indicated a decline in substrate quality and microbial activity with secondary forest succession. The concentration of total phenols in mineral soil showed no significant trend with TSF, but was negatively correlated (R2=0.486, P=0.025) with resin sorbed NO3- concentration indicating either enhanced immobilization or perhaps chemical inhibition. These results imply that biochemical processes (decomposition and N transformations) may be limited by the lack of available substrate and potentially as a result of rapid immobilization, chemical inhibition or a combination of both at least partially induced by changes in vegetation with TSF. Our results suggest that N availability in ponderosa pine ecosystems of the inland Northwest are directly dependent upon fire history and secondary successional stage..
机译:对于蒙大拿州西部低海拔森林的防火如何影响氮(N)循环的了解甚少。尚不清楚森林管理导致的火灾频率变化如何从植物-土壤-微生物相互作用的角度影响生态系统功能。火灾时间序列方法用于研究森林演替对自火灾(2-130年)以来不同时间的10个地点的土壤生化特性和微生物活性的影响。发现自火灾发生以来,埋藏的压舌板和棉条的分解速率显着下降(分别为R2 = 0.410,P = 0.087和R2 = 0.761,P = 0.003)。用树脂吸附的NH4 +和NO3-浓度估算的净氮矿化和硝化作用,在TSF中均表现出明显的非线性下降(分别为R2 = 0.870,P = 0.000和R2 = 0.620,P = 0.007)。使用充气土壤淤浆法测得的硝化潜能,TSF也显着降低(R2 = 0.595,P = 0.009)。 N有效性的这些降低,以及代谢商的增加和TSF不稳定的C库的减少表明,次生森林演替会导致底物质量和微生物活性下降。矿物土壤中总酚的浓度与TSF没有明显关系,但与树脂吸附的NO3-浓度呈负相关(R2 = 0.486,P = 0.025),表明固定化或化学抑制作用增强。这些结果表明,生化过程(分解和N转化)可能会由于缺乏可用的底物而受到限制,并且可能是由于快速固定,化学抑制或至少部分由TSF植被变化引起的两者结合的结果。我们的结果表明,西北内陆的黄松林生态系统中的氮有效性直接取决于火灾历史和次生演替阶段。

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