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Influences of thinning, prescribed burning, and wildfire on soil processes and properties in southwestern ponderosa pine forests: a retrospective study.

机译:稀疏,规定的燃烧和野火对西南美国黄松林的土壤过程和特性的影响:一项回顾性研究。

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Following Euro-American settlement in the late 1800s, fire suppression and livestock grazing in ponderosa pine-bunchgrass ecosystems of the southwestern US resulted in the replacement of grass openings with dense stands of ponderosa pine. This, in turn, has led to apparent decreases in decomposition, net N mineralization, and soil respiration (i.e., net soil CO2 efflux) rates, losses of floral and faunal diversity, and greater risk of the occurrence of stand-replacing wildfire. Alterations in ecosystem structure and function have prompted the implementation of restoration treatments throughout the region. Using a retrospective approach, we investigated the effects of thinning, thinning plus prescribed fire, and wildfire, 6-15 years following treatments, on ecosystem processes and properties across a 750-km2 area in northern Arizona, USA. We found that stands that had thinning or thinning plus burning treatments had lower in situ annual rates of net N mineralization in the mineral soil than unmanaged stands. However, stands burned by high-severity wildfire had net N mineralization rates that were approximately 60% higher than unmanaged stands. Because of similarities in net N mineralization rates among treatments under laboratory conditions, we speculate that variation in in situ net N transformation rates among stands were due to differences in C inputs (thinned and thinned plus burned) and soil microclimate (wildfire) among the stands. Size of the soil microbial C and N pools generally declined with decreases in litterfall (highest in unmanaged, intermediate in thinned and thinned plus burned, and lowest in wildfire stands); however, in situ rates of net soil CO2 efflux did not follow this pattern. Our results contrast with some previous studies in southwestern ponderosa pine (Pinus ponderosa var. arizonica and scopulorum) forests where restoration treatments (both thinning and thinning plus burning) increased net N transformation rates. We hypothesize that the dissimilarity in responses to treatments across studies is due to differences in the relative effect of these treatments on the quantity and quality of C inputs. Large increases in easily decomposable understorey biomass following restoration treatments appear to result in increases in N cycling rates, whereas treatments that result in either no change or minimal increases in understorey biomass, accompanied by a long-term decrease in pine needle input to the forest floor, lead to reductions in N cycling rates. We recommend that restoration and fire-hazard reduction treatments be applied preferentially to stands that currently have low understorey production..
机译:在1800年代末期的欧美定居之后,美国西南部的美国黄松-松草生态系统中的灭火和放牧导致草木被茂密的黄松林代替。反过来,这导致分解,净氮矿化和土壤呼吸(即土壤净二氧化碳排放量)速率明显降低,花和动物多样性的丧失,以及发生替代林地的大火的风险。生态系统结构和功能的改变促使整个地区实施恢复治疗。使用回顾性方法,我们研究了处理后6至15年间间伐,间伐加规定的火和野火对美国亚利桑那州北部750平方公里地区生态系统过程和特性的影响。我们发现,经过稀疏或稀疏再加上燃烧处理的林分,其矿质土壤中净氮矿化的原位年均生长速率低于未管理林分。但是,被高强度野火燃烧的林分的净氮矿化率比未经管理的林分高约60%。由于实验室条件下各处理之间净氮矿化率的相似性,我们推测林分间原位净氮转化率的变化是由于林分间碳输入(稀薄和稀薄加上燃烧)和土壤小气候(野火)的差异所致。 。土壤微生物碳和氮库的大小通常随着凋落物的减少而减少(未管理的最高,稀疏和稀薄加燃烧的中等,野火林最低);然而,土壤净CO2外排的原位速率没有遵循这种模式。我们的结果与之前在西南美国黄松(Pinus tankerosa var。arizonica和scopulorum)森林中进行的一些研究形成对比,在这些森林中,恢复处理(间伐和间伐加燃烧)提高了净氮转化率。我们假设不同研究对治疗的反应差异是由于这些治疗对C输入的数量和质量的相对影响不同所致。复原处理后易于分解的底层生物量的大量增加似乎导致氮循环速率的增加,而处理导致底层生物量无变化或最小增加的处理,伴随着长期松针输入林地的减少,导致N循环速率降低。我们建议优先对目前底层产量较低的林地进行恢复和减少火灾隐患的处理。

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