Yang Zhi Min, Liu Xin Min
College of Life Science and Technology, Inner Mongolia Normal University, Huhhot 010022, China.
Wudan Mongulia Nationality Middle School of Ongniud Bannar, Chifeng 024500, Inner Mongolia, China.
Ying Yong Sheng Tai Xue Bao. 2016 Sep;27(9):2864-2874. doi: 10.13287/j.1001-9332.201609.033.
Grazing has been considered to be an important factor determining the composition of soil animals and decomposition of leaf litter in grassland ecosystem. Sampling plots were selected in ungrazed grassland, grazed grassland and sandy land. Litter bags were used to compare the changes of physicochemical properties of Stipa grandis litter and the composition of soil fauna in the process of the litter decomposition in Baiyinxile, Inner Mongolia, since 2010 to 2012. A total number of 67056 soil animals were captured, belonging to five phyla and eight classes, including 23 families of mites and 19 families of insects. After 780 days' decomposition, the loss of the organic matter of S. grandis litter was from 92.5% to 40.0% in the ungrazed grassland, and to 41.3% in the grazed grassland, with no significant difference observed. However, there was a significant difference (P<0.05) between the ratio of litter residues of the ungrazed grassland (50.0%) and that of the grazed grassland (23.0%). The abundance of soil animals in the residual litters was significantly decreased in the grazed grassland compared to the ungrazed grassland. When the litter was moved into the sandy land, the decomposition rate of organic matter in the residual litter was not significant changed but the ratio of litter residue declined significantly, and the composition of mite community in the resi-dual litter changed significantly. Our results illustrated that grazing activity could affect the composition and abundance of soil fauna in temperate grassland, but slightly influenced the decomposition of organic matter. Therefore, soil animals had relatively weak direct effects on the decomposition of litter in this semi-arid region.
放牧被认为是决定草原生态系统中土壤动物组成和凋落物分解的一个重要因素。在未放牧草地、放牧草地和沙地选取了样地。自2010年至2012年,在内蒙古白音锡勒,利用凋落物袋比较了大针茅凋落物理化性质的变化以及土壤动物在凋落物分解过程中的组成。共捕获67056只土壤动物,分属于5个门8个纲,包括23科螨类和19科昆虫。经过780天的分解,大针茅凋落物的有机质损失在未放牧草地为92.5%至40.0%,在放牧草地为41.3%,未观察到显著差异。然而,未放牧草地(50.0%)和放牧草地(23.0%)的凋落物残留率之间存在显著差异(P<0.05)。与未放牧草地相比,放牧草地残留凋落物中的土壤动物丰度显著降低。当将凋落物移至沙地时,残留凋落物中有机质的分解速率没有显著变化,但凋落物残留率显著下降,残留凋落物中螨类群落的组成也发生了显著变化。我们的结果表明,放牧活动会影响温带草原土壤动物的组成和丰度,但对有机质分解的影响较小。因此,在这个半干旱地区,土壤动物对凋落物分解的直接影响相对较弱。