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Effect of warming and grazing on litter mass loss and temperature sensitivity of litter and dung mass loss on the Tibetan plateau

机译:温牧对青藏高原凋落物质量损失及凋落物和粪便质量损失温度敏感性的影响

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Knowledge about the role of litter and dung decomposition in nutrient cycling and response to climate change and grazing in alpine ecosystems is still rudimentary. We conducted two separate studies to assess the relative role of warming and grazing on litter mass loss and on the temperature sensitivity of litter and dung mass loss. Experiments were conducted for 1-2 years under a controlled warming-grazing system and along an elevation gradient from 3200 to 3800 m. A free-air temperature enhancement system (FATE) using infrared heaters and grazing significantly increased soil temperatures (average 0.5-1.6 degrees C) from 0 to 40 cm depth, but neither warming nor grazing affected soil moisture except early in the growing seasons at 30 cm soil depth. Heaters caused greater soil warming at night-time compared with daytime, but grazing resulted in greater soil warming during daytime compared with night-time. Annual average values of the soil temperature at 5 cm were 3.2, 2.4 and 0.3 degrees C at 3200, 3600 and 3800 m, respectively. Neither warming nor grazing caused changes of litter quality for the first year of the controlled warming-grazing experiment. The effects of warming and grazing on litter mass losses were additive, increasing litter mass losses by about 19.3% and 8.3%, respectively, for the 2-year decomposition periods. The temperature sensitivity of litter mass losses was approximately 11% degrees C-1 based on the controlled warming-grazing experiment. The annual cumulative litter mass loss was approximately 2.5 times that of dung along the elevation gradient. However, the temperature sensitivity (about 18% degrees C-1) of the dung mass loss was about three times that of the litter mass loss. These results suggest greater warming at night-time compared with daytime may accelerate litter mass loss, and grazing will enhance carbon loss to atmosphere in the region through a decrease of litter biomass and an increase of dung production with an increase of stocking rate in future warmer conditions.
机译:关于凋落物和粪便分解在养分循环中的作用以及对高山生态系统中气候变化和放牧的反应的知识仍然很初级。我们进行了两项单独的研究,以评估升温和放牧对凋落物质量损失以及凋落物和粪便质量损失的温度敏感性的相对作用。实验是在受控的放牧系统下并沿3200至3800 m的海拔梯度进行的,为期1-2年。使用红外加热器和放牧的自由空气温度增强系统(FATE)从0到40厘米深度显着提高了土壤温度(平均0.5-1.6摄氏度),但除生长季节初期30摄氏度外,升温和放牧都不会影响土壤水分厘米土壤深度。与白天相比,加热器在夜间导致更大的土壤变暖,但与白天相比,放牧导致白天的土壤变暖更大。 5 cm处土壤温度的年平均值分别为3200、3600和3800 m,分别为3.2、2.4和0.3摄氏度。在受控的温草试验的第一年,变暖和放牧都不会引起垫料质量的变化。加温和放牧对凋落物质量损失的影响是累加的,在两年的分解期内,凋落物质量损失分别增加了约19.3%和8.3%。根据受控的温草试验,垫料质量损失的温度敏感性约为11%C-1。沿海拔梯度,年累积凋落物质量损失约为粪便质量损失的2.5倍。但是,粪便质量损失的温度敏感性(大约18%C-1)是垃圾质量损失的三倍。这些结果表明,与白天相比,夜间变暖更大,可能会加速垃圾质量的损失,放牧将通过减少垃圾生物量和增加粪便产量,从而增加该地区向大气中的碳损失,而未来变暖的话,放养率也会增加条件。

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