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Productivity and Quality of Alpine Grassland Vary With Soil Water Availability Under Experimental Warming

机译:试验升温条件下高寒草地生产力随土壤水分的变化而变化

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摘要

The plant productivity of alpine meadow is predicted to generally increase under a warming climate, but it remains unclear whether the positive response rates will vary with soil water availability. Without consideration of the response of community composition and plant quality, livestock grazing under the current stocking rate might still lead to grassland degradation, even in meadows with high plant biomass. We have conducted a warming experiment from 2010 to 2017 to examine the interactive effects of warming and soil water availability on plant growth and forage quality at individual and functional group levels in an alpine meadow located in the permafrost region of the Qinghai–Tibetan Plateau. Warming-induced changes in community composition, biomass, and forage quality varied with soil water availability. Under dry conditions, experimental warming reduced the relative importance of grasses and the aboveground biomass by 32.37 g m−2 but increased the importance value of forbs. It also increased the crude fat by 0.68% and the crude protein by 3.19% at the end of summer but decreased the acid detergent fiber by 5.59% at the end of spring. The increase in crude fat and protein and the decrease in acid detergent fiber, but the decrease in aboveground biomass and increase the importance value of forbs, which may imply a deterioration of the grassland. Under wet conditions, warming increased aboveground biomass by 29.49 g m−2 at the end of spring and reduced acid detergent fiber by 8.09% at the end of summer. The importance value of grasses and forbs positively correlated with the acid detergent fiber and crude protein, respectively. Our results suggest that precipitation changes will determine whether climate warming will benefit rangelands on the Qinghai–Tibetan Plateau, with drier conditions suppressing grassland productivity, but wetter conditions increasing production while preserving forage quality.
机译:预计在气候变暖的情况下,高寒草甸的植物生产力通常会提高,但尚不清楚阳性反应率是否会随土壤水分的利用而变化。如果不考虑社区组成和植物质量的响应,即使在植物生物量较高的草地上,以目前的放养率放牧的牲畜仍可能导致草原退化。我们从2010年至2017年进行了一项变暖实验,研究了青藏高原多年冻土区高寒草甸中变暖和土壤水分有效性对个体和功能组水平上植物生长和饲草质量的相互作用。气候变暖引起的群落组成,生物量和牧草质量的变化随土壤水的可用性而变化。在干燥条件下,实验性升温使草类和地上生物量的相对重要性降低了32.37 g m -2 ,但增加了草的重要性。在夏季末,它还使粗脂肪增加了0.68%,使粗蛋白增加了3.19%,但在春季末使酸性洗涤剂纤维减少了5.59%。粗脂肪和蛋白质的增加以及酸性洗涤剂纤维的减少,但地上生物量的减少和草的重要性增加,这可能意味着草原的退化。在潮湿的条件下,春季末变暖使地上生物量增加了29.49 g m −2 ,夏季末使酸性洗涤剂纤维减少了8.09%。草和草的重要性值分别与酸性洗涤剂纤维和粗蛋白成正相关。我们的结果表明,降水变化将决定气候变暖是否会使青藏高原的牧场受益,干旱的天气会抑制草地的生产力,而潮湿的天气会增加产量,同时又保持草料的质量。

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