Converting acidic forests to managed plantations reduces soil nitrogen loss by inhibiting autotrophic nitrification while inducing nitrate immobilization in the tropics

IF 5.1 1区 农林科学 Q1 SOIL SCIENCE
Qilin Zhu, Ahmed S. Elrys, Lijun Liu, Yunxing Wan, Ruoyan Yang, Jinxia Mou, Yunzhong Chen, Yuqin Wang, Juan Liu, Tongbin Zhu, Yanzheng Wu, Shuirong Tang, Lei Meng, Jinbo Zhang, Christoph Müller
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Abstract

Soil gross nitrogen (N) transformation rates are highly sensitive to land use change. However, understanding the effect of land use change on internal N cycling patterns and its underlying mechanisms in tropical soils remains elusive. Here, four typical land uses including forest (> 400 years), eucalyptus (15 years), rubber (35 years), and paddy field (40 years) plantations in tropical region of China were investigated. The technique of 15N tracing was used to quantify soil gross N transformation rates. We also measured soil biochemical properties as well as carbon (C) and N fractions to evaluate the controls on any changes in soil N cycling processes. We found that converting natural tropical forests to managed ecosystems shifts the soil N dynamics from nitrate-dominated N forms towards ammonium-dominated N forms, suggesting that managed ecosystems becoming conservative (i.e., lower ratio of autotrophic nitrification (ONH4) to ammonium immobilization (INH4) and nitrous oxide (N2O) emissions and higher nitrate immobilization) than the natural tropical forest. The higher tendency of N loss (i.e., higher ONH4/INH4 and N2O emissions) of the natural tropical forest was mainly due to the higher concentrations of soil total N and hydrolysable ammonium N and microbial biomass, which stimulated ONH4. Lower microbial biomass, hydrolysable ammonium N, particulate organic C, and gross N mineralization, however, significantly decreased ONH4 in managed ecosystems. Our study also showed a pivotal role of soil C and N fractions in controlling soil heterotrophic nitrification, which enhanced significantly with decreasing amino sugar N, amino acid N, dissolved organic C, easily oxidizable organic C, and light fraction organic C. Our findings highlighted the pivotal role of soil C and N fractions in regulating soil N cycling under future land use changes.

Abstract Image

在热带地区,将酸性森林转化为有管理的人工林通过抑制自养硝化作用和诱导硝酸盐固定来减少土壤氮的流失
土壤总氮(N)转化率对土地利用变化高度敏感。然而,土地利用变化对热带土壤内部氮循环模式的影响及其潜在机制尚不明确。这里有四种典型的土地用途,包括森林(>对中国热带地区400年的桉树人工林(15年)、橡胶人工林(35年)和水田人工林(40年)进行了调查。采用15N示踪技术定量测定土壤总氮转化速率。我们还测量了土壤生化特性以及碳(C)和氮组分,以评估对土壤氮循环过程变化的控制。我们发现,将天然热带森林转化为管理生态系统将使土壤N动态从硝酸盐主导的N形式转变为氨主导的N形式,这表明管理生态系统比天然热带森林变得保守(即自养硝化(ONH4)比铵固定化(INH4)和氧化亚氮(N2O)排放的比例更低,硝酸盐固定化的比例更高)。热带天然林氮损失的增加趋势(即ONH4/INH4和N2O排放量的增加)主要是由于土壤全氮、水解铵态氮和微生物生物量的增加刺激了ONH4。微生物生物量、可水解铵态氮、颗粒有机碳和总氮矿化显著降低了管理生态系统的ONH4。研究还表明,土壤C和N组分在控制土壤异养硝化中的关键作用,随着氨基糖N、氨基酸N、溶解性有机C、易氧化性有机C和轻组分有机C的降低,异养硝化作用显著增强。研究结果表明,在未来土地利用变化下,土壤C和N组分在调节土壤N循环中的关键作用。
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来源期刊
Biology and Fertility of Soils
Biology and Fertility of Soils 农林科学-土壤科学
CiteScore
11.80
自引率
10.80%
发文量
62
审稿时长
2.2 months
期刊介绍: Biology and Fertility of Soils publishes in English original papers, reviews and short communications on all fundamental and applied aspects of biology – microflora and microfauna - and fertility of soils. It offers a forum for research aimed at broadening the understanding of biological functions, processes and interactions in soils, particularly concerning the increasing demands of agriculture, deforestation and industrialization. The journal includes articles on techniques and methods that evaluate processes, biogeochemical interactions and ecological stresses, and sometimes presents special issues on relevant topics.
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