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Redistribution of Extractable Nutrients Following Disc Trenching on Luvisols and Brunisols in Saskatchewan

机译:在萨斯喀彻温省的圆盘沟对卢维索尔和布鲁尼索尔进行盘沟处理后,可提取营养物的重新分布

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摘要

Disc trenching is an important silvicultural management tool for cre-ating microsites to ensure the survival and growth of newly planted seedlings. Mounded microsites are thought to be a source ofnutrients for seedling roots; however, little is known concerning how nutrients are redistributed in the soil after disc trenching. Theobjective of this study, therefore, was to determine the redistribution of soil horizons and selected soil chemical properties fol-lowing Delta disc trenching. Three sites were selected on both Luvisol and Brunisol soils in northern Saskatchewan. Soil profileswere excavated and samples collected from 15 × 15 cm grids to a 1-m depth. Samples were analyzed for pH and extractable nitrate(NO ), ammonium (NH ), phosphorus (P), potassium (K) and sulfur (S). Disc trenching concentrated extractable N, P and S in the 34berm microsite compared to the trench microsites. The redistribution of extractable NO , NH and P in the berms compared to the 34trench microsites was 20 times greater for Luvisol sites compared to the Brunisol sites, while extractable K and S were similar between both microsites for each soil. Seedlings planted on these mounded microsites therefore should have a large pool of nutri- ents for plant growth; however, further work is needed to determine patterns of nutrient uptake by seedlings in relation to mound- ed and trench microsites.
机译:盘式挖沟是用于创建微型站点的重要营林管理工具,可确保新种植的幼苗的生存和生长。堆肥的微场所被认为是幼苗根部营养的来源。然而,人们对圆盘挖沟后如何在土壤中重新分配养分知之甚少。因此,本研究的目的是确定在Delta盘式挖沟之后土壤层位的重新分布和选定的土壤化学性质。在萨斯喀彻温省北部的Luvisol和Brunisol土壤上均选择了三个地点。挖掘土壤剖面,并从15×15 cm的网格中收集样品至1 m深度。分析样品的pH值和可萃取的硝酸盐(NO),铵(NH),磷(P),钾(K)和硫(S)。与沟槽式微场所相比,圆盘式沟槽在34层微场所中集中浓缩了可提取的N,P和S。与34沟微地点相比,护堤中可提取的NO,NH和P的重新分布比Lunissol地点的Luvisol地点高20倍,而每种土壤的两种地点之间的可提取K和S相似。因此,在这些丘陵微地上种植的幼苗应具有大量植物生长所需的营养;然而,还需要进一步的工作来确定幼苗相对于丘陵和沟渠微地点的养分吸收方式。

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