MA Chengzhong1, DENG Jifeng1, 2. Effects of Different Planting Densities of Mongolian Pine on the Soil Particle Size Characteristics in Southern Mu Us Desert[J]. 2017, 31(1): 230-235.
MA Chengzhong1, DENG Jifeng1, 2. Effects of Different Planting Densities of Mongolian Pine on the Soil Particle Size Characteristics in Southern Mu Us Desert[J]. 2017, 31(1): 230-235. DOI: 10.13870/j.cnki.stbcxb.2017.01.038.
探讨樟子松人工林林下土壤粒度特征随林分密度的变化及影响,以期为毛乌素沙地以樟子松为建群种的植物固沙模式提供理论依据。以陕西省榆林市珍稀沙生植物保护基地内8个密度梯度(925~2 700 株/hm2)的沙地樟子松人工林为研究对象,分别采集0—20,20—40 cm 2层土壤样本,测定土壤粒度组成,计算分析平均粒径、标准偏差、偏度、峰态值和分形维数。结果表明:研究区各层土壤粒度组成以砂粒为主,其次是粉粒、黏粒;粒度特征整体呈现粒径较粗、分选较差、偏态正和峰态为中至窄的特点,土壤分形维数分布于1.422~2.084之间;樟子松林林下各层土壤平均粒径和分形维数均大于裸沙地,且随着林分密度的增加,平均粒径和分形维数均呈现递增趋势,而樟子松林林下各层土壤偏度均小于裸沙地,且随着林分密度的增加,呈现递减趋势,说明土壤细粒物质在樟子松林下的长期保护下逐渐恢复,并且表层土壤恢复速度大于下层土壤;同时,随林分密度的增大,标准偏差和峰态值没有明显的规律,土壤颗粒的粗细分配变化不稳定,说明林分密度因素不足以致使土壤颗粒的粗细分配朝良好趋势发展。
Abstract
To reveal the effects of artificial Mongolian pine forest on soil particle size parameters in southern Mu Us desert
soil samples (taken as two layers 0—20 cm and 20—40 cm) under different plant densities (925~2 700 plants/hm2) as well as the bare sand land (control check) were selected in Yulin rare desert plant protection base of Shaanxi Province. Soil particle size parameters such as average particle size
standard deviation
skewness
kurtosis and fractal dimension were identified and calculated by using laser diffraction technique. The results showed that in the study area
majority soil particle size was occupied by sand particles
followed by silt particles and then clay particles. Soil particle size parameters presented comparatively thick
poor sorting
positive skewness as well as middle or sharp kurtosis. Fractal dimension of soil was in range of 1.422~2.084. As affected by Mongolian pine plantation
the average particle size and fractal dimension values were continue to increase leading to constantly particle distribution optimization than that of bare sand land
especially in the top layer of soil profile
such effects were more obvious. Meanwhile
there were no obvious regularities in standard deviation and kurtosis along with the increase of stand density. And distribution of soil particles was not balance. The results indicated that stand density factor was not enough to cause the thickness distribution of soil particles toward the trend of balance.