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Reforestation and slope-position effects on nitrogen, phosphorus pools, and carbon stability of various soil aggregates in a red soil hilly land of subtropical China

机译:再造林和坡位对亚热带红壤丘陵区土壤团聚体中氮,磷库和碳稳定性的影响

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摘要

The impact of slope position on forest restoration processes may dominate the interaction among topsoil aggregates, nutrients, and organic carbon (C) stability following reforestation on degraded hilly land. Six paired plots of shrubland and Masson pine (Pinus massoniana Lamb.) plantation reforested on shrubland were selected at different positions along a 25 degrees slope in subtropical China. Soil and ecosystem nitrogen (N), phosphorus (P), and organic C stocks were quantified using a combination of excavation, harvest, and modeling methods. Carbon stability in differently sized soil aggregates was measured using dry sieving and closed-jar alkali-absorption methods. Reforestation increased total ecosystem C, N, and P stocks, but did not alter soil C and P stocks, and decreased N stocks at 0-75 cm soil depth by 18%. The shift from shrubland to forests increased organic C stability for various soil aggregates, particularly with a mean increase of 34% and 30% at lower and middle slope positions, respectively. The slope-position effect was largely attributable to the increased mean mass diameter of soil aggregates and the reduced organic C mineralization potential in larger soil aggregates relative to smaller soil aggregates. Soil aggregates had more stable organic C in forests than in shrubland due to increase in the carbon to nitrogen (C/N) and carbon to phosphorus (C/P) ratios with reforestation. Slope position influenced restoration effectiveness in the red soil hilly region.
机译:在退化的丘陵地带上重新造林后,斜坡位置对森林恢复过程的影响可能主导着表土聚集体,养分和有机碳(C)稳定性之间的相互作用。在亚热带地区,沿25度坡度在不同位置选择了6个成对的灌木丛和马尾松(Pinus massoniana Lamb。)人工林。土壤和生态系统中的氮(N),磷(P)和有机碳储量采用挖掘,收获和建模方法相结合的方法进行了定量。使用干筛和密闭碱吸收法测量了不同大小的土壤团聚体中的碳稳定性。植树造林增加了生态系统中C,N和P的总蓄积量,但并未改变土壤C和P的蓄积量,并且在0-75厘米土壤深度下减少了18%的N储量。从灌木丛到森林的转变增加了各种土壤团聚体的有机碳稳定性,​​尤其是在较低和中等坡度位置分别增加了34%和30%。坡位效应主要归因于相对于较小的土壤团聚体,较大的土壤团聚体的平均质量直径增加和有机碳矿化潜力降低。由于造林后碳氮(C / N)和碳磷(C / P)比的增加,森林土壤中的团聚体比灌木丛中的有机碳更稳定。斜坡位置影响了红壤丘陵区的修复效果。

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