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 densityplantations of Pinus sylvestris L. Var. mongolica Litv. in the southeast of Mu Us Sandland. For thepurpose of evaluating the hydrological function of litter and soil quantitatively, 30 standard plots (10types of forest×3 replications) were investigated. The soil physical characteristics and water-holdingcapacity were determined. The results showed that: (1) The total storage capacity of litter among 10forest 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 nosignificant differences in water content, bulk density and the maximum water-holding capacity of soilamongst 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 variedgreatly with a variation range of 0.99-4.32%. The hydrological effects of soil were the highest in theP III and P IV plots, and the lowest in the P I plot. (3) The power function model can better indicate highcorrelation coefficients between the water absorption rate of litter and its immersion time, and alsobetween the water-holding capacity of litter and its soaking time. The stable infiltration rates of soil in10 different forest stands were consistent, while they varied greatly with a range of 0.11-0.89 mm/minafter 20 minutes. (4) In this study, the hydrological effects of forest litter and soil in P III and P IV plotswere the best, and the optimal afforestation density was 1500 to 1800 plants per hectare. The resultsshow that thinning should be done timely and appropriately in this study area to prevent the recessionof a forest stand. Besides, it is unapproachable whether Pinus sylvestris Var. mongolica can beplanted in large scale or in high density, and further research is needed.
机译:在樟子松不同种植密度下进行凋落物和土壤层的水文效应的初步研究。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)。确定了土壤的物理特性和持水能力。结果表明:(1)在10种森林类型中,凋落物的总存储量通常为P III = P IV> PX> P VII> P IX> P VI> P VII> PV> P II> PI; 10种森林类型的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,土壤含水量,容重和最大持水量之间无显着差异,变化范围为8.94-16.54%,1.10-1.66 g / cm 3和200.43-266.43 t / hm。 2个。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%。在P III和P IV地块中,土壤的水文效应最高,而在P I地块中,最低。 (3)幂函数模型可以较好地表明垃圾的吸水率与浸泡时间之间的相关系数较高,并且可以更好地说明垃圾的保水能力与浸泡时间之间的相关系数。 10个不同林分土壤的稳定入渗速率是一致的,但在20分钟后它们的变化很大,范围为0.11-0.89 mm / min。 (4)在本研究中,P III和P IV样地的森林凋落物和土壤的水文效应最佳,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,樟子松是否变种也是不可取的。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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