Results 21 to 30 of about 172,067 (173)

利用15N揭示滴灌区盐旱胁迫对土壤氮素分布与棉花生长的影响

open access: yesShuitu Baochi Xuebao, 2021
为了探究盐旱胁迫对土壤中氮素分布和棉花生长的影响,通过测坑试验研究滴灌区不同盐分、干旱条件下土壤全氮、硝氮、氨氮的分布和棉花生长情况。试验设置3种盐分梯度的土壤(电导率,EC):3,6,9 dS/m,分别用T1、T2、T3表示;3个灌水量:2 700,3 600,4 500 m3/hm2,分别用W1、W2、W3表示(4 500 m3/hm2为当地推荐灌水量)。结果表明:当土壤盐分梯度> 3 dS/m时土壤全氮累积量显著高于低盐土壤(P<0.05),且土壤盐分对棉花花期生长影响较大 ...
冯玥   +7 more
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Lithology modulates soil priming effect via resource limitations and bacterial community structure

open access: yesFunctional Ecology, Volume 40, Issue 1, Page 176-190, January 2026.
Read the free Plain Language Summary for this article on the Journal blog. Abstract The soil priming effect (PE), triggered by root exudate inputs that stimulates microbial activity and drives significant soil carbon (C) losses in terrestrial ecosystems.
Xinyu Hou   +4 more
wiley   +1 more source

杨凌地区大棚土壤硝态氮累积效应研究

open access: yesShuitu Baochi Xuebao, 2008
通过调查不同棚龄大棚土壤硝态氮含量的变化,研究了杨凌大棚蔬菜生产中的土壤硝态氮累积特性,结果显示:大棚蔬菜土壤硝态氮含量显著高于露天菜地和拱棚土壤,反映出过高的氮肥投入,各棚龄土壤均表现出明显的硝态氮表土累积。随着棚龄的增加土壤硝态氮及总盐含量呈增加趋势,土壤pH值则表现为逐渐下降,不合理的施肥将导致短龄大棚土壤硝态氮及总盐含量急剧上升而超过长龄大棚土壤;在番茄生长周期内随生育期延长硝态氮在土壤中累积量逐渐增大,但总盐含量变化并不明显。硝态氮在土壤中的迁移,导致土壤底层硝态氮也大量累积。
魏迎春, 李新平, 刘刚, 朱辉娟
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模拟氮沉降对华北落叶松人工林土壤微生物碳和微生物氮的动态影响

open access: yesShuitu Baochi Xuebao, 2020
为揭示过量的大气氮沉降对华北落叶松人工林土壤微生物碳、氮和土壤呼吸的影响,通过对照(N0:0 g/(m2·a))、轻度施氮(N1:8 g/(m2·a))、重度施氮(N2:15 g/(m2·a))3个外源施氮水平下5年的野外定点试验和观测,模拟过量氮沉降条件下华北落叶松人工林土壤微生物碳、氮和土壤呼吸的变化,旨在阐明林下土壤微生物和呼吸对过量氮沉降的响应及其对土壤碳氮循环的影响。结果表明:在5—10月生长季中,土壤微生物碳和氮的平均含量分别为1 098.93,97.31 mg/kg ...
李素新   +3 more
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Factors influencing fine roots decomposition rates in response to nitrogen addition vary across root characteristics

open access: yesFunctional Ecology, Volume 39, Issue 12, Page 3504-3516, December 2025.
Read the free Plain Language Summary for this article on the Journal blog. Abstract Nitrogen (N) deposition strongly affects litter decomposition and nutrient release, thereby reshaping carbon cycling in terrestrial ecosystems. Although most studies have focused on above‐ground litter, the effects of N addition on fine root decomposition and their ...
Yuneng Wang   +5 more
wiley   +1 more source

富士苹果营养转换期肥料氮去向和土壤氮库盈亏研究

open access: yesShuitu Baochi Xuebao, 2017
运用15N同位素示踪技术,以5年生烟富3/SH6/平邑甜茶苹果为试材,研究了不同施氮水平(0,50,100,150,200,250 kg/hm2)对营养转换期富士苹果肥料氮吸收利用、土壤残留和土壤氮库盈亏的影响。结果表明,随施氮水平的提高,肥料氮的利用率逐渐下降,且树体吸收土壤氮素的比例逐渐降低,而来自肥料氮的比例逐渐升高;施氮1个月后,5.75%~12.99%的肥料氮被树体吸收,29.62%~39.74%的肥料氮残留在0—60 cm土体中,47.27%~64.64%的肥料氮通过其他途径损失 ...
王 芬   +6 more
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Nitrogen‐transforming microorganisms potentially facilitate the invasion of Moso bamboo (Phyllostachys edulis) into evergreen broadleaf forests

open access: yesFunctional Ecology, Volume 39, Issue 10, Page 2704-2716, October 2025.
Read the free Plain Language Summary for this article on the Journal blog. Abstract Moso bamboo (Phyllostachys edulis) invasions into broadleaf forests can cause serious ecological problems, such as reducing biodiversity and disrupting community succession.
Ting Zhou   +5 more
wiley   +1 more source

祁连山东段青海云杉林区土壤氮矿化与土壤因子的相关性

open access: yesShuitu Baochi Xuebao, 2016
以祁连山东段青海云杉(Picea crassifolia)林分布带土壤为研究对象,采用顶盖埋管的野外取样法和室内分析法,对海拔梯度上土壤铵态氮(NH4+-N)、硝态氮(NO3--N)净矿化速率、氮净矿化量和净矿化速率进行测定分析,旨在探讨土壤净氮矿化量与气温降水和土壤理化性质的相关关系,以期建立环境变量与土壤氮矿化量和矿化速率模型,进而提高祁连山青海云杉林生产力及水源涵养能力。结果表明:(1)土壤硝态氮、铵态氮净矿化速率、土壤净氮矿化量和矿化速率随海拔的升高差异性均极显著 ...
张, 李, 车宗玺, 王, 刘贤德
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Arbuscular mycorrhizal fungus reshapes the rhizosphere microbiome of alfalfa in response to above‐ground attack by aphids and a fungal plant pathogen

open access: yesFunctional Ecology, Volume 39, Issue 8, Page 2149-2169, August 2025.
Read the free Plain Language Summary for this article on the Journal blog. Abstract Plants assemble beneficial rhizosphere microbiomes through a ‘cry for help’ mechanism upon pathogen or insect herbivore attack. The arbuscular mycorrhizal fungi (AMF) can influence the composition of microbial communities in the plant rhizosphere. However, their impacts
Yingde Li   +6 more
wiley   +1 more source

黄土区几种土壤培养过程中可溶性有机氮的变化及其与土壤矿化氮的关系

open access: yesShuitu Baochi Xuebao, 2008
研究了黄土高原12种土壤(农地和林地)35 d好气培养过程中可溶性有机氮(SON)含量及其占可溶性全氮(TSN)的比例,以及SON与土壤矿化氮间的关系。结果表明,随着培养过程的进行,不同类型土壤SON的含量均呈明显增加;土壤SON占TSN的比例在培养的前3 d内明显下降,随后这一比例基本保持在24%左右。根据总可溶性氮确定的供试土壤氮素矿化势No平均为45.8 mg/kg,较由矿化的无机氮确定的土壤氮素矿化势No(平均36.5 mg/kg)高约1/4左右 ...
赵满兴, Kalbitz, Karsten, 周建斌
doaj  

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