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Impact of Exotic Earthworms on Organic Carbon Sorption on Mineral Surfaces and Soil Carbon Inventories in a Northern Hardwood Forest

机译:北方硬木森林中外来Earth对矿物表面有机碳吸附和土壤碳库的影响

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Exotic earthworms are invading forests in North America where native earthworms have been absent since the last glaciation. These earthworms bioturbate soils and may enhance physical interactions between minerals and organic matter (OM), thus affecting mineral sorption of carbon (C) which may affect C cycling. We quantitatively show how OM-mineral sorption and soil C inventories respond to exotic earthworms along an earthworm invasion chronosequence in a sugar maple forest in northern Minnesota. We hypothesized that mineral surface area in A horizons would increase as burrowing earthworms incorporated clay minerals from the B horizons and that enhanced contacts between OM and minerals would increase the OM sorption on mineral surfaces and mineral-associated C inventories in A horizons. Contrary to our hypotheses, mineral surface areas within A horizons were lowered because earthworm burrows only extended into the silt-rich loess that separated the A and clay-rich B horizons. Furthermore, where endogeic earthworms were present, a smaller fraction of mineral surface area was covered with OM. OM sorption on minerals in the A horizons shifted from a limitation of mineral surface availability to a limitation of OM availability within a decade after the arrival of endogeic earthworms. C-mineral sorption depends on earthworm consumption of OM as well as the composition and vertical distribution of minerals. This finding may thus explain the contradictory results reported in earlier investigations. Our results highlight the rapid and drastic effects of exotic earthworms on key ecosystem processes in deciduous forests in post-glacial settings.
机译:自上次冰川消融以来,外来earth就已入侵北美的森林。这些earth使土壤生物紊乱,并可能增强矿物质与有机物(OM)之间的物理相互作用,从而影响碳对矿物质的吸收(C),这可能会影响C的循环。我们定量地显示了在明尼苏达州北部的枫树森林中,OM矿物吸附和土壤C清单如何沿着worm入侵的时间序列响应外来earth。我们假设A层的矿物表面积会增加,因为穴居会结合B层的粘土矿物,而OM与矿物之间的增强接触会增加OM在A层矿物表面和与矿物相关的C清单上的吸附。与我们的假设相反,A层内的矿物表面积降低了,因为worm洞穴仅延伸到了将A和B层隔开的富含粉土的黄土中。此外,在存在内endo的地方,一小部分的矿物质表面积被OM覆盖。在内生earth到来的十年之内,A层矿物对OM的吸附从矿物表面可利用性的局限性转变为OM可利用性的局限性。 C-矿物质的吸收取决于worm对OM的消耗以及矿物质的组成和垂直分布。因此,这一发现可以解释早期调查中报道的矛盾结果。我们的研究结果突显了外来earth对冰川期后落叶森林关键生态系统过程的快速而剧烈的影响。

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