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添加氮和磷会改变水杉人工林中土壤的氮转化。

Nitrogen and phosphorus additions alter soil N transformations in a Metasequoia glyptostroboides plantation.

作者信息

Zhang Youzheng, Jiang Pengcheng, Guo Yaolin, Wu Ming, Shao Xuexin, Xu Hengtao, Wu Tonggui, Yuan Wenwen, Li Niu

机构信息

Key Laboratory of Engineering Oceanography, Key Laboratory of Nearshore Engineering Environment and Ecological Security of Zhejiang Province, Second Institute of Oceanography, Ministry of Natural Resources, Hangzhou, China.

Wetland Ecosystem Research Station of Hangzhou Bay, Research Institute of Subtropical Forestry, Chinese Academy of Forestry, Hangzhou, China.

出版信息

Front Plant Sci. 2024 Aug 27;15:1448356. doi: 10.3389/fpls.2024.1448356. eCollection 2024.

Abstract

INTRODUCTION

Nitrogen (N) and phosphorus (P) enrichment due to anthropogenic activities can significantly affect soil N transformations in forest ecosystems. However, the effects of N and P additions on nitrification and denitrification processes in plantations, and economically important forest type in China, remain poorly understood.

METHODS

This study investigated the responses of soil nitrification and denitrification rates, as well as the abundances of nitrifiers and denitrifiers, to different levels of N and P additions in a 6-year nutrient addition experiment in a plantation.

RESULTS

Stepwise multiple regression analysis was used to identify the main predictors of nitrification and denitrification rates. The results showed that moderate N addition (N2 treatment, 2.4 mol·m) stimulated nitrification rates and abundances of ammonia-oxidizing archaea (AOA) and bacteria (AOB), while excessive N and P additions inhibited denitrification rates and reduced the abundance of -type denitrifiers. AOB abundance was the main predictor of nitrification rates under N additions, whereas microbial biomass carbon and nirS gene abundance were the key factors controlling denitrification rates. Under P additions, tree growth parameters (diameter at breast height and crown base height) and AOB abundance were the primary predictors of nitrification and denitrification rates.

DISCUSSION

Our study reveals complex interactions among nutrient inputs, plant growth, soil properties, and microbial communities in regulating soil N transformations in plantation forests. This study also offers valuable insights for formulating effective nutrient management strategies to enhance the growth and health of plantations under scenarios of increasing elevated nutrient deposition.

摘要

引言

人为活动导致的氮(N)和磷(P)富集可显著影响森林生态系统中的土壤氮转化。然而,在中国一种重要的经济型森林类型——人工林中,氮和磷添加对硝化和反硝化过程的影响仍知之甚少。

方法

本研究在一项为期6年的人工林养分添加实验中,调查了土壤硝化和反硝化速率以及硝化菌和反硝化菌丰度对不同水平氮和磷添加的响应。

结果

采用逐步多元回归分析来确定硝化和反硝化速率的主要预测因子。结果表明,适度添加氮(N2处理,2.4 mol·m)刺激了硝化速率以及氨氧化古菌(AOA)和细菌(AOB)的丰度,而过量添加氮和磷则抑制了反硝化速率并降低了Ⅱ型反硝化菌的丰度。在添加氮的情况下,AOB丰度是硝化速率的主要预测因子,而微生物生物量碳和nirS基因丰度是控制反硝化速率的关键因素。在添加磷的情况下,树木生长参数(胸径和冠基高)和AOB丰度是硝化和反硝化速率的主要预测因子。

讨论

我们的研究揭示了养分输入、植物生长、土壤性质和微生物群落在调节人工林土壤氮转化中的复杂相互作用。本研究还为在养分沉降增加的情况下制定有效的养分管理策略以促进人工林生长和健康提供了有价值的见解。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/6208/11384580/ebd4f76fb436/fpls-15-1448356-g001.jpg

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