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Condition of Forest Soils Under Plantations Of Scots Pine of Various Age in the Forest-Steppe Zone of Trans-Ural

机译:在跨国林草原区苏格兰苏格兰森林地区森林土壤条件

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The paper contains an analysis of fertility changes in dark gray forest soils under man-made forests of Pinus sylvestris (L.) with the age of 15; 30; 45 and 60 years. The studies were performed in the territory of a forest enterprise located in Abatsky district of Tyumen oblast, in the northern forest-steppe of Western Siberia. Dark gray forest soil under a birch forest was used as a control. It has been established, that change in type of forest cover leads to changes in the species composition of the grass and shrub stratum. Humus state of the dark gray forest soils under man-made pine forests gradually deteriorates. Humus content reduces to 5.4% in the case where pines reach 60 years of age, while in the control plot under natural vegetation it amounts to 7.4% of soil mass. Qualitative composition of humus also gradually deteriorates: A fulvate-humate type is substituted with a humate-fulvate one, with low nitrogen enrichment. It has been established, that leaching is amplified under man-made pine forests with the age of under 45 years. Subsequently (60 years), podzolization starts in the dark gray forest soil, manifesting as destruction of soil adsorbing complex and increased acidity of the humus layer. In 45 years, base saturation decreased from 77% to 71% of the cation exchange capacity. Change in the humus state and chemical properties had a negative impact onto agrophysical properties of the dark gray forest soil. Water stability of structural aggregates gradually reduces from 65 to 42% with increased age of pine, while bulk density increases to 1.27 g/cm3. To prevent loss of fertility soils in Northern Trans-Ural, it is recommended to thoroughly analyze the plots planned under coniferous trees, to avoid their planting onto dark gray forest soils or soils similar in fertility. When moving such soils into arable lands, special measures are required for radical improvement in fertility (application of fertilizers, chalking) with subsequent sowing of perennial herbs.
机译:本文含有5岁的人造森林下深灰色森林土壤的生育变化分析; 30; 45和60年。这些研究在位于西伯利亚西部北部森林干草原的秋森州北部的Abatsky地区的森林企业境内进行。桦木森林下的深灰色森林土壤被用作控制。已经建立,森林覆盖类型的变化导致草和灌木层的物种组成的变化。人造松树林下深灰色森林土壤的腐殖质逐渐恶化。腐殖质含量在50岁以下的情况下减少到5.4%,而在天然植被下的控制图中,它占土壤质量的7.4%。腐殖质的定性组成也逐渐恶化:富含腐殖型被腐蚀 - 富含腐蚀,具有低富集富集。已经建立,浸出在人造的松树林下,年龄不到45岁。随后(60岁),潮汐型开始于深灰色林土土壤,表现为破坏土壤吸附复合物的复杂和腐殖质层的酸度。 45年来,基础饱和度从阳离子交换能力的77%降至71%。腐殖质状态和化学性质的变化对深灰色林土土壤的农药性质产生负面影响。结构聚集体的水稳定性随着松树年龄而增加的65%至42%,而散装密度增加到1.27g / cm3。为了防止北方尿布中的生育土壤损失,建议彻底分析针叶树下计划的地块,以避免其种植在肥沃的灰色森林土壤或土壤中的生育率。当移动这样的土壤为耕地,都需要在生育与多年生草本植物的播种以后彻底改善(肥料的应用,粉化)的特殊措施。

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