首页> 外文期刊>Nature environment and pollution technology >Hydrological Effects of Forest Litter and Soil on Different Density Plantations of Pinus sylvestris L Var. mongolica Litv. in Mu Us Sandland, Northwest China
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Hydrological Effects of Forest Litter and Soil on Different Density Plantations of Pinus sylvestris L Var. mongolica Litv. in Mu Us Sandland, Northwest China

机译:森林凋落物和土壤对不同密度的樟子松人工林的水文影响。蒙古自治州在中国西北部的姆斯沙地

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A pilot study of hydrological effects of litter and soil layers was carried out on different density plantations of Pinus sylvestris L. Var. mongolica Litv. in the southeast of Mu Us Sandland. For the purpose of evaluating the hydrological function of litter and soil quantitatively, 30 standard plots (10 types of forest×3 replications) were investigated. The soil physical characteristics and water-holding capacity were determined. The results showed that: (1) The total storage capacity of litter among 10 forest types, generally followed by the sequence of forest densities, were P_Ⅲ = P_Ⅳ > P_Ⅹ > P_Ⅶ > P_Ⅸ > P_Ⅵ > P_Ⅶ >P_Ⅴ > P_Ⅱ > P_Ⅰ; the maximum water-holding capacity and effective water-holding capacity of litter, for 10 forest types, were 2.46-8.23 t/hm~2 and 0.163-6.42 t/hm~2, respectively. (2) There were no significant differences in water content, bulk density and the maximum water-holding capacity of soil amongst these forest types, with the variation range of 8.94-16.54%, 1.10-1.66 g/cm~3 and 200.43-266.43 t/hm~2, respectively. However, the non-pore porosity of soil among these 10 forest types varied greatly with a variation range of 0.99-4.32%. The hydrological effects of soil were the highest in the P_Ⅲ and P_Ⅳ plots, and the lowest in the P_Ⅰ plot. (3) The power function model can better indicate high correlation coefficients between the water absorption rate of litter and its immersion time, and also between the water-holding capacity of litter and its soaking time. The stable infiltration rates of soil in 10 different forest stands were consistent, while they varied greatly with a range of 0.11-0.89 mm/min after 20 minutes. (4) In this study, the hydrological effects of forest litter and soil in P_Ⅲ and P_Ⅳ plots were the best, and the optimal afforestation density was 1500 to 1800 plants per hectare. The results show that thinning should be done timely and appropriately in this study area to prevent the recession of a forest stand. Besides, it is unapproachable whether Pinus sylvestris Var. mongolica can be planted in large scale or in high density, and further research is needed.
机译:对樟子松不同密度人工林凋落物和土壤层的水文影响进行了初步研究。蒙古自治州在Mu Us Sandland的东南部。为了定量评估枯枝落叶和土壤的水文功能,研究了30个标准样地(10种森林类型×3个重复样地)。测定土壤的物理特性和持水能力。结果表明:(1)10种森林类型凋落物的总存储量,通常依次为森林密度P_Ⅲ=P_Ⅳ>P_Ⅹ> P_ P>P_Ⅸ>P_Ⅵ>P_Ⅶ>P_Ⅴ>P_Ⅱ>P_Ⅰ; 10种森林类型凋落物的最大持水量和有效持水量分别为2.46-8.23 t / hm〜2和0.163-6.42 t / hm〜2。 (2)在这些森林类型中,水分,容重和最大持水量之间没有显着差异,变化范围为8.94-16.54%,1.10-1.66 g / cm〜3和200.43-266.43 t / hm〜2。然而,这10种森林类型中土壤的非孔隙孔隙度变化很大,变化范围为0.99-4.32%。土壤水文效应在P_Ⅲ和P_Ⅳ图中最高,而在P_Ⅰ图中最低。 (3)幂函数模型可以更好地说明垃圾的吸水率与浸泡时间之间的相关系数高,以及垃圾的持水量与浸泡时间之间的相关系数高。 10个不同林分土壤的稳定入渗率是一致的,但在20分钟后它们的变化很大,范围为0.11-0.89 mm / min。 (4)本研究以P_Ⅲ和P_Ⅳ地块的森林凋落物和土壤水文效应最佳,最佳造林密度为每公顷1500至1800株植物。结果表明,在该研究区应及时,适当地进行疏伐,以防止林分衰退。此外,樟子松是否变质也是不可取的。蒙古可以大规模或高密度种植,需要进一步的研究。

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