科尔沁固定沙地植被特征对降雨变化的响应
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中国科学院寒区旱区环境与工程研究所,中国科学院寒区旱区环境与工程研究所,中国科学院寒区旱区环境与工程研究所,中国科学院寒区旱区环境与工程研究所,中国科学院寒区旱区环境与工程研究所,中国科学院寒区旱区环境与工程研究所

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国家自然科学基金项目(41371053);国家科技支撑计划项目(2011BAC07B02);中国科学院战略性先导科技专项(XDA05050201-04-01)


Response of sandy vegetation characteristics to precipitation change in Horqin Sandy Land
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Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences,,,,,

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    摘要:

    选择科尔沁固定沙地利用一种野外增减雨试验装置研究了沙地植被生长特征对降雨增减变化的响应。结果表明:(1)在6月,降雨增减变化对植物群落高度有显著影响(P < 0.05)。减雨60%和30%时,植物群落平均高度比对照分别降低8.8%和2.3%,增雨60%和30%时,则分别增加6.8%和1.4%;相比增雨60%,增雨30%更能促进群落盖度的增大;降雨量变化影响群落植株密度。(2)1a的降雨增减变化对沙地植被的多样性和均匀度均没有显著影响,但减雨可显著增加7月物种的丰富度(P < 0.05)。(3)随着降雨量的增加,地上生物量逐渐增大,在增雨30%时达到最大值;而地下生物量会随着降雨量增加而显著增大,同时,减雨60%也使地下生物量增加。此外,降雨量的增加和减少都会使地下与地上生物量的比值增加。(4)固定沙地地下生物量主要分布在0-20 cm之间,占总地下生物量的52.7%;降雨量的增加显著增加20-40 cm土壤中根系的分布,当降雨量减少60%时,20-40 cm土壤中根系的分布也略有增加,增雨60%和减雨60%对地下生物量在40-60 cm土层的分布具有明显的促进作用。

    Abstract:

    Precipitation plays an important role in vegetation establishment and plant growth, species composition and community structure and biomass distribution. With the intensification of global climate change, the effect of annual rainfall and its pattern on vegetation is getting more important. To clarify the response of sandy vegetation to precipitation (P) change,a device was used in a field experiment to control precipitation amount in Horqin Sandy Land. The height, density and coverage, species composition, above-ground and below-ground biomass of the vegetation were surveyed at 48 quadrates (50 cm×50 cm) once a month from May to July. The results showed that (1) Change of P had a significant effect on the average height, density and coverage of the sandy land vegetation. The rainfall in May is 19.2 mm and the coverage is higher in the plots with P added by 30% than that reduced by 30% and 60%, significantly. And there is a significant difference between P addition by 60% and reduction by 30%. When P added by 60%, the average density was deceased by 15.4%, but it was increased by 15.3% when P reduced by 30% compared with the control. In June, the rainfall was 96.8 mm, when P reduced by 60% and 30%, the average height was decreased by 8.8% and 2.3%, respectively. and the average height was increased by 6.8% and 1.4% when P added by 60% and 30%, respectively. The coverage is higher when P added by 30% than reduced by 30% significantly, and the vegetation coverage, compared with the control, was correspondingly increased by 19.7% and decreased 60.5%, respectively. Coverage was significantly increased in plots with P added by 60% than that reduced by 60%. The average plant density was increased by 8.90% when P added by 30%, and decreased by 14.2% while P added by 60%. (2) The effect of P change on diversity index and evenness was not significant within one year but the abundance index was influenced significantly in only July. There is a significant difference between P reduction by 30% and addition by 30% and 60%. The species richness presented a decrease trend with P addition. (3) P change had a significant effect on the aboveground biomass. When P added by 30%, the aboveground biomass was increased and maximized at 167.94 g/m2 and the minimum was 68.37 g/m2. The underground biomass was increased significantly with P addition. The ratio of underground biomass to aboveground biomass of all treatments was increased. (4) The underground biomass of the sandy land vegetation was mainly distributed in 0-20 cm and 20-40 cm soil layers, accounted for 52.7% and 42.65%, respectively. The distribution of roots in 20-40 cm soil layer was increased significantly with P addition, and increased slightly when P reduced by 60%. The underground biomass in 40-60 cm was increased when P reduced by 60% and added by 60%.

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张腊梅,刘新平,赵学勇,张铜会,岳祥飞,云建英.科尔沁固定沙地植被特征对降雨变化的响应.生态学报,2014,34(10):2737~2745

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