首页|植被恢复对退化红壤水稳性团聚体有机碳的影响

植被恢复对退化红壤水稳性团聚体有机碳的影响

Effects of vegetation restoration on water-stable aggregate organic carbon in degraded red soil

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为从微观角度揭示植被恢复对土壤结构的影响,采用野外调查与室内分析相结合的方法,研究南方红壤退化地3种典型植被恢复类型[马尾松与阔叶复层林(PB)、 木荷×马尾松混交林(SP)、 阔叶林(BF)]土壤(0~60 cm土层)水稳性团聚体有机碳分布特征及其对总有机碳的贡献率.结果表明:土壤水稳性团聚体含量及其有机碳贡献率随团聚体粒径的减小总体呈"W"或"N"字分布;不同粒径水稳性团聚体含量以粒径<0.05 mm占优势,而大粒径团聚体含量在湿筛过程中大幅降低,表明大粒径团聚体在水的浸润中更易受到影响;上层土壤(0~40cm)水稳性大团聚体(粒径>0.25 mm)总含量均以PB最高,而在下层土壤(40~60 cm)3种植被恢复类型较为接近(48.80%~51.64%).土壤总有机碳和水稳性团聚体有机碳含量大小顺序均表现为PB>SP>BF,随着土层深度的增加,两者均呈下降趋势;水稳性大团聚体有机碳含量总体高于微团聚体(粒径<0.25 mm),说明有机碳对水稳性大团聚体的形成具有积极作用.不同林分土壤团聚体有机碳贡献率均以粒径0.05~0.25 mm最小,且PB中粒径>2.00 mm的团聚体有机碳贡献率显著高于SP和BF(P<0.05).保留密度大、 灌木(草)层盖度高的马尾松与阔叶复层林土壤水稳性大团聚体与团聚体有机碳含量更高,对土壤结构改善与功能恢复效果更好.
To reveal effects of vegetation restoration on soil structure at the molecular scale, three typical vegetation restoration types in degraded red soil were selected which were Pinus massoniana-broadleaved multiple layer forest ( PB ) , Schima superba-Pinus massoniana mixed forest (SP) and broad-leaved forest (BF), respectively.Using field investigations and lab assays to investigate the distribution characteristics and contribution rate of soil water-stable aggregate organic carbon in 0~60 cm soil layers in each of the three types.The results showed that the soil water-stable aggregate content and the contribution rate of the aggregate organic carbon were distributed as"W"or"N"with the reduction of aggregate particle size;particles less than 0.05 mm in diameter made up the majority of water-stable aggregates in soil, and the macro-aggregate content reduced rapidly when water-sieving which suggested that the macro-aggregates were more susceptible to water infiltration; the water-stable aggregate content of particles more than 0.25 mm in upper soil layers (0~40 cm) was the highest in PB while the content in lower soil layer ( 40~60 cm) was relatively close ( 48.80%~51.64%) among three types.The content of soil total organic carbon and water-stable aggregate organic carbon were ranked as PB>SP>BF exhibiting reductions with the increase of soil depth; the organic carbon contents of macro water-stable aggregates were higher than those of micro water-stable aggregates (<0.25 mm in diameter ) suggesting that organic carbon may play an active role in the formation and the water-stability of macro aggregates.The contribution rate of soil aggregate organic carbon of particle in 0.05~0.25 mm was minimum in all the three types, and the contribution rate of soil aggregate organic carbon of particle more than 2.00 mm in PB was significantly higher than that in SP and BF ( P<0.05) .PB had the highest macro water-stable aggregates and aggregate organic carbon content among the three types which can be attributed to the high density and coverage of understory shrubs/herbs in PB, and it was more conducive to the improvement of the soil structure and function.

vegetation restorationwater-stable aggregateorganic carbonred soil

朱丽琴、黄荣珍、贾龙、黄国敏、王赫、刘勇

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南昌工程学院江西省退化生态系统修复与流域生态水文重点实验室, 江西南昌330099

植被恢复 水稳性团聚体 有机碳 红壤

国家自然科学基金江西省自然科学基金江西省高等学校"十二五"水土保持与荒漠化防治重点学科培育基金

3116017920151BAB204033

2018

森林与环境学报
福建农林大学

森林与环境学报

CSTPCDCSCD北大核心
影响因子:0.964
ISSN:2096-0018
年,卷(期):2018.38(1)
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