Effects of exotic plant invasion on soil nitrogen availability

外来植物入侵对土壤氮循环和氮有效性的影响是入侵成功或进一步加剧的重要原因。通过对比相同研究地点入侵区域和无入侵区域的土壤原位氮状态差异, 探讨了外来植物入侵对土壤氮有效性的影响程度和生理生态学机制。基于107篇相关研究文献数据的整合, 发现植物入侵区域相对于无入侵区域土壤总氮、铵态氮、硝态氮、无机氮、微生物生物量氮含量显著增加, 增幅分别为(50 ± 14)%、(60 ± 24)%、(470 ± 115)%、(69 ± 25)%、(54 ± 20)%。土壤硝态氮含量增幅较大反映硝化作用增强, 这可能增加入侵植物硝态氮利用以及喜硝植物的共存。温带地区植物入侵后土壤的硝态氮含量增幅显著高于亚热带地区。固氮植物入侵后土壤的总氮和无机氮含量增幅均显著高于非固氮植物入侵。木本和常绿植物入侵后土壤的总氮含量增幅分别高于草本和落叶植物入侵; 而土壤铵态氮含量的增幅没有显著差异且与固氮入侵植物占比无明显关系; 然而硝态氮含量的增幅普遍较高且与固氮入侵植物占比显著正相关。外来入侵植物固氮功能以及凋落物质量和数量是影响土壤氮矿化和硝化过程的关键因素。该研究为理解外来植物入侵成功和加剧的机制以及入侵植物功能性状与土壤氮动态之间的关系提供了新的见解。     

北方农牧交错带温性盐碱化草地土壤呼吸对不同形态氮添加和刈割的响应

农牧交错带草地生态系统兼受农业和牧业的影响, 属于脆弱生态系统, 尤其是养分贫瘠的盐碱化草地, 其生态系统结构和功能对外界干扰的响应更加强烈。位于晋西北地区的农牧交错带盐碱化草地, 地理位置独特, 区别于天然牧区草地生态系统。由于毗邻农田, 农业氮肥的过量使用促进了活性氮气体排放, 同时使得农牧交错带草地土壤碳氮循环发生改变。刈割是北方农牧交错草地生态系统的主要管理方式, 为了深入探究氮添加和刈割管理方式对农牧交错带草地碳循环的影响, 进一步厘清该区域草地生态系统的碳动态问题, 该研究设置了一个不同形态氮添加和刈割的裂区实验, 测定土壤呼吸对不同形态氮肥添加和刈割的响应, 为进一步科学管理该区域草地提供可靠的依据。实验样地位于山西省右玉县境内的“山西农业大学农牧交错带草地生态系统野外观测研究站”, 于2017年设置不同形态氮添加和刈割处理, 实验处理包括对照(不刈割和刈割)、尿素添加、缓释尿素添加、刈割+尿素添加、刈割+缓释尿素添加, 每种处理6个重复, 共36个小区。在不同处理条件下测定土壤呼吸速率、土壤温度、土壤水分、土壤微生物生物量、土壤无机氮含量、植物地上和地下生物量, 并计算土壤累积碳排放量及CO₂通量。研究结果表明: (1)短期(2017-2018年)尿素和缓释尿素的添加显著提高了该地区土壤呼吸速率和土壤累积碳排放量。与添加缓释尿素相比, 添加尿素处理下的土壤呼吸速率和累积碳排放量更高; (2)刈割显著降低土壤呼吸速率和累积碳排放量; (3)短期氮添加和刈割的交互作用对土壤呼吸速率没有显著影响。因此, 短期氮添加促进了北方农牧交错带盐碱化草地土壤碳释放, 刈割抑制土壤呼吸, 降低了累积碳排放量, 这可能是由于刈割移除地上植物, 减少了凋落物的输入, 底物减少导致土壤微生物活性降低。但是随着处理时间的延长, 氮添加和刈割对该农牧交错带盐碱化草地土壤碳动态的影响还有待进一步探究和发现。     

Effects of calcium fertilizer on yield,quality and related enzyme activities of peanut in acidic soil

AimsPeanut (Arachis hypogaea) is one of the calcium (Ca)-like crops. In acidic soil, low soil exchangeable Ca²⁺ content, which usually is caused by eluviation, can affect peanut pod development, even causes pod unfilled. The objective of this study was to investigate the effects of calcium fertilizer on yield, quality and related enzyme activities of peanut in acidic soil.Methods ‘Huayu22’ was used as materials, and field experiments were conducted in Wendeng, Weihai (2013) and Sanzhuang, Rizhao (2014), respectively. Three treatments were carried out, i.e. No Ca-application (T₀), 14 kg·667 m^-2 fused CaO (T₁) and 28 kg·667 m^-2 fused CaO (T₂). Top 3rd leaves of main stems were harvested to determine the activities of carbon and nitrogen metabolism enzyme every 15 days from anthesis to mature period. Additionally, the pod traits and yield were investigated at harvest time. Uniform dry pods were used to determine the quality of kernel.Important findings Application of calcium fertilizer significantly increased the pod yield of peanut in acid soil. Yield of T₁ treatment increased by 26.92% and T₂ increased by 21.65% on average at two sites. It might be related to higher pod numbers per plant, higher double kernel rate, and higher plumpness of kernel under T₁ and T₂ treatment than under T₀ treatment. Simultaneously, application of calcium fertilizer also significantly increased the protein and fat content of peanut in acidic soil. The protein content increased 2.02% and the fat content increased 3.01% on average in T₁ treatment, respectively. The protein content increased 1.56% and the fat content increased 2.58% in T₂ treatment, respectively. Additionally, Calcium fertilizer not only improved the lysine and total amino acid content but also improved oleic/linoleic acid (O/L) ratio of peanut in acidic soil. These might be due to higher activities of glutamine synthetase (GS), glutamate synthetase (GOGAT) and glutamate pyruvate transaminase (GPT) in the leaves of peanut in acidic soil under T₁ and T₂ treatments than under T₀ treatment. What’s more, the activity of GS of peanut treated with T₁ was higher than that treated with T₂. Application of Calcium fertilizer also improved the activities of phosphoenolpyruvate carboxylase (PEPCase), sucrose synthase (SS) and sucrose phosphate synthase (SPS) of peanut at early growing period, but the activities at late growth stage were lower than T₀ treatment. Our results demonstrate that the economic performance of 14 kg·667 m^-2 fused CaO was the best one among these three treatments applied.     

Responses of soil respiration with biocrust cover to water and temperature in the southeastern edge of Tengger Desert,Northwest China

Aims Soil respiration of the lands covered by biocrusts is an important component in the carbon cycle of arid, semi-arid and dry-subhumid ecosystems (drylands hereafter), and one of the key processes in the carbon cycle of drylands. However, the responses of the rate of soil respiration with biocrusts to water and temperature are uncertain in the investigations of the effects of experimental warming and precipitation patterns on CO₂ fluxes in biocrust dominated ecosystems. The objectives of this study were to investigate the relationships of carbon release from the biocrust-soil systems with water and temperature in drylands. Methods Intact soil columns with two types of biocrusts, including moss and algae-lichen crusts, were collected in a natural vegetation area in the southeastern fringe of the Tengger Desert. Open top chambers were used to simulate climate warming, and the soil respiration rate was measured under warming and non-warming treatments using an automated soil respiration system (LI-8150). Important findings Over the whole observational period (from April 2016 to July 2016), soil respiration rates varied from -0.16 to 4.69 μmol·m^-2·s^-1 for the moss crust-covered soils and from -0.21 to 5.72 μmol·m^-2·s^-1 for the algae-lichen crust-covered soils, respectively, under different rainfall events (the precipitations between 0.3-30.0 mm). The mean soil respiration rate of the moss crust-covered soils is 1.09 μmol·m^-2·s^-1, which is higher than that of the algae-lichen crust-covered soils of 0.94 μmol·m^-2·s^-1. The soil respiration rate of the two types of biocrust-covered soils showed different dynamics and spatial heterogeneities with rainfall events, and were positively correlated with precipitation. The mean soil respiration rate of the biocrust-covered soils without warming was 1.24 μmol·m^-2·s^-1, significantly higher than that with warming treatments of 0.79 μmol·m^-2·s^-1 (p < 0.05). By increasing the evaporation of soil moisture, the simulated warming impeded soil respiration. In most cases, soil temperature and soil respiration rate displayed a similar single-peak curve during the diel cycle. Our results show an approximately two hours’ lag between soil temperature at 5 cm depth and the soil respiration rate of the biocrust-covered soils during the diel cycle.     

氮硅添加对青藏高原高寒草甸土壤氮矿化的影响

为了解全球气候变化背景下氮沉降对土壤氮矿化的影响及硅添加对土壤氮矿化的促进作用, 该试验设置不同浓度的氮肥单独添加(0、20、40、60 g·m ^-2, 分别为对照CK、N20、N40、N60)以及与硅肥配施(硅酸4 g·m ^-2, Si4), 测定不同处理下0-20、20-40、40-60 cm土层土壤硝态氮含量、铵态氮含量、净硝化速率、净氨化速率以及净矿化速率。结果显示: (1)单独添加氮肥, 各土层土壤硝态氮和铵态氮含量均随处理浓度的增加而增加, 0-20 cm土层N20、N40、N60处理下土壤硝态氮和铵态氮分别较CK增加63.48%、126.04%、247.03%和80.66%、152.52%、244.56%; 随着土层深度增加, 土壤硝态氮、铵态氮含量均有下降, 20-40、40-60 cm土层较0-20 cm土层硝态氮含量分别平均减少53.90%、76.05%, 铵态氮含量分别平均减少48.62%、68.23%。(2)土壤净硝化速率、净氨化速率及净矿化速率随着氮肥浓度增加均呈上升趋势。相同氮肥添加浓度下, 土壤净硝化速率、净氨化速率和净矿化速率随着土层深度增加逐渐下降(除CK外)。(3)与单独添加氮肥比较, 氮硅肥配施, 土壤氮含量有显著提高, 在0-20 cm土层硝态氮和铵态氮较CK分别增加98.78%、192.62%、330.16%和99.96%、195.82%、306.32%, 20-40、40-60 cm土层也有类似趋势。同时, 氮硅配施促进了土壤氮矿化行为, 在0-20 cm土层, N60Si4处理下的土壤净硝化速率、净氨化速率较单独施氮时分别增加35.88%、27.41%。以上结果表明, 与单独氮肥添加相比, 氮硅配施不但能提高土壤氮含量, 而且能促进土壤氮的矿化作用, 对大气氮沉降有一定的缓解作用。     

亚热带人工林下植被根际土壤酶化学计量特征

为探讨林下植被根际土壤酶化学计量特征及其对林分类型和季节的响应, 该研究以江西省泰和县千烟洲试验站典型人工杉木(Cunninghamia lanceolata)、马尾松(Pinus massoniana)和湿地松(Pinus elliottii)林林下优势灌草檵木(Loropetalum chinense)、杨桐(Adinandra millettii)、格药柃(Eurya muricata)、狗脊蕨(Woodwardia japonica)和暗鳞鳞毛蕨(Dryopteris atrata)为对象, 在植被生长初期(4月)和旺盛期(7月)测定优势灌草根际土壤与碳(C)循环相关的β-1,4-葡萄糖苷酶(BG)、与氮(N)循环相关的β-1,4-N-乙酰葡糖氨糖苷酶(NAG)和亮氨酸氨基肽酶(LAP)、与磷(P)循环相关的酸性磷酸酶(AP)活性、酶化学计量比及土壤理化性质。结果发现: (1)根际土壤与C和N循环相关的酶活性以及BG:AP (酶C:P)在不同林下植被之间存在显著差异, 而与P循环相关的酶活性差异不显著。林分类型和取样季节显著影响BG:(NAG+LAP)(酶C:N), 且林下植被类型、林分类型和取样季节交互影响酶C:P。主成分分析表明, 根际土壤酶的活性及计量比在不同林下植被(檵木不同于格药柃, 且二者显著区别于其他物种)、林分类型(杉木林区别于马尾松、湿地松林)和取样季节之间均存在显著差异。土壤硝态氮(NO₃ ^--N)、铵态氮(NH₄ ⁺-N)、可溶性有机碳(DOC)含量和碳氮比(C:N)是影响林下植被根际土壤酶的活性及化学计量比的主要因素。(2)标准主轴回归分析表明, 林下植被根际土壤lg(BG)、lg(NAG+LAP)和lg(AP)之间存在显著线性关系, lgBG:lg(NAG+LAP):lgAP (酶C:N:P)约为1:1:1.3, 酶C:P及(NAG+LAP):AP (酶N:P)分别为0.14和0.15。AP远大于BG和NAG+LAP的活性, 导致lg(BG)和lg(NAG+LAP)与lg(AP)的回归斜率极显著偏离1。说明林下植被根际土壤酶的活性及计量比受植被种类、林分类型及取样季节影响, 且基质有效性在其中发挥重要作用。相较于C循环和N循环, 微生物会分配更多资源用于P循环相关酶的生产, 暗示亚热带人工林林下植被根际土壤微生物生长和活性更易受P限制。     

山东滨海盐碱地11个造林树种叶解剖特征对土壤条件的响应

叶片作为植物与大气环境连接的重要纽带, 对逆境具有强烈的响应。基于叶性状探讨植物对环境的适应机制对盐碱地植物群落构建具有指导意义。该研究以山东省滨海盐碱地3种不同土壤条件下的11个造林树种为对象, 通过对各树种叶解剖性状的测定分析, 阐明叶片功能性状与盐碱地土壤环境的关系, 以期为盐碱地植被修复与群落构建提供科学依据。主要研究结果: (1) 11个树种的叶片厚度较大, 栅栏组织发达, 紧密排列在叶肉近轴面, 呈3-5层。各树种叶片的栅栏组织与海绵组织厚度比值(PT/ST)普遍较高但差异较大, 可指示叶解剖特征在树种间的差异性。(2)不同树种的叶解剖结构在立地环境间具有显著差异, PT/ST可作为指示指标。(3)相关分析和冗余分析表明, 树种叶片解剖结构与立地土壤条件具有密切联系。PT/ST与土壤理化性质相关程度高, 且与土壤pH以及土壤电导率(25 ℃)均呈显著正相关关系, 与土壤硝态氮含量呈显著负相关关系。叶片特征和叶脉特征可解释叶性状随环境变异约84%的信息量。综上所述,叶解剖结构与盐碱地土壤条件存在密切关系, 基于叶解剖特征可进一步分析树种对盐碱环境的适应性, 并为盐碱地植物群落构建的树种选择提供科学依据。     

摩西斗管囊霉改善连作花生根际土壤的微环境

花生(Arachis hypogaea)长期连作导致土壤环境恶化, 严重影响产量和品质。丛枝菌根真菌(AMF)作为有益真菌能够与80%的陆生植物根系形成共生关系, 这种共生体能够改善植物根系微环境, 提高植物对营养物质的吸收和对逆境胁迫的抗性。为了探究AMF对花生连作土壤微环境的影响, 该研究通过对花生连作土壤接种和未接种摩西斗管囊霉(Funneliformis mosseae)试验, 在花生不同生长期检测根际土壤的酶活性、土壤矿物质含量、土壤微生物群落结构和多度的变化情况, 以及对连作花生产量和品质的影响。研究结果表明: 1)摩西斗管囊霉能够显著提高花生根际土壤蔗糖酶、脲酶、碱性磷酸酶和硝酸还原酶的活性; 2)摩西斗管囊霉显著增加花生连作土壤中全氮、全磷、全钾、速效磷和速效钾的含量; 3)摩西斗管囊霉显著降低土壤中有害真菌曲霉菌属(Aspergillus)的多度, 减少镰刀菌属(Fusarium)和赤霉菌属(Gibberella)的多度, 但是没有达到显著水平, 显著增加有益细菌放线菌Gaiella属的多度; 4)摩西斗管囊霉显著提高连作花生的产量, 增加籽仁中蛋白质、油酸和亚油酸的含量。因此, 摩西斗管囊霉能够改善连作花生根际土壤微生态环境, 增强连作土壤对致病菌的抵抗能力, 从而缓解连作障碍对花生根系的危害。     

模拟增温对荒漠生物土壤结皮-土壤系统CO2、CH4和N2O通量的影响

目前, 有关增温条件下荒漠生物土壤结皮(BSCs)-土壤系统与大气之间主要温室气体(CO₂、CH₄和N₂O)通量变化的研究十分匮乏, 以致很难准确地评估荒漠生态系统温室气体通量对气候变暖的响应与反馈的方向和程度。该文选择腾格里沙漠东南缘天然植被区由藻类、藓类以及二者混生的3种类型的BSCs覆盖土壤为研究对象, 以开顶式生长室(OTC)为增温方式模拟全球变暖, 采用静态箱-气相色谱法探究了2012年7月至2013年6月增温和不增温处理下CO₂、CH₄和N₂O通量的变化特征。结果表明: 增温和结皮类型对CO₂、CH₄和N₂O通量没有显著影响。采样日期、结皮类型与采样日期, 以及增温与结皮类型和采样日期的互作显著影响CO₂和CH₄通量, 增温和采样日期互作显著影响CH₄通量。BSCs-土壤系统的CO₂、CH₄和N₂O年通量及其增温潜能在增温和不增温处理下的差异均不显著。CO₂通量与5 cm深度的土壤温度呈显著的指数正相关关系, 与10 cm深度的土壤湿度呈线性正相关关系; 藓类、混生结皮的CH₄通量与5 cm深度的土壤温度和10 cm深度的土壤湿度均呈显著的线性负相关关系; 3种结皮类型的N₂O通量与5 cm深度的土壤温度均无相关关系, 藓类结皮的N₂O通量与10 cm深度的土壤湿度呈显著的线性负相关关系。藓类结皮的CO₂和CH₄在增温和不增温两种处理下的通量差异与5 cm深度的土壤温度差异呈显著的负线性相关, 藻类结皮N₂O的通量差异与温度差异呈近似正相关关系(p = 0.051)。以上结果说明: 在全球变暖的背景下, 荒漠BSCs-土壤系统主要温室气体通量不会有明显的变化, 意味着荒漠生态系统温室气体的排放可能对气候变暖没有明显的 反馈。     

长期不同植被覆盖对黑土团聚体内有机碳组分的影响

为探究黑土团聚体内土壤有机碳(SOC)的“分馏”特征, 揭示不同植被覆盖下土壤团聚体的固碳机制, 该文以中国科学院海伦农业生态系统国家野外综合研究站内不同植被覆盖(草地、农田和裸地)长期定位实验的土样为研究对象, 利用团聚体湿筛分组、有机碳物理和化学分组相结合的方法, 研究了黑土团聚体及其内部的碳密度和腐殖质组分的碳分配特征。研究发现, 黑土经过不同植被覆盖31年后, 长期草地覆盖使土壤表层SOC、全氮(TN)含量显著增加, 农田和无植被覆盖的裸地SOC含量减少, 且在裸地显著降低。3种处理中, 2-0.25 mm (含2 mm, 下同)粒级团聚体均为优粒级。土壤团聚体的稳定性顺序为草地>农田>裸地。草地覆盖使土壤大团聚体的比例和有机碳库增加, 微团聚体和粉黏粒所占比例和碳库均减少, 说明草地覆盖促进了土壤大团聚体形成, 土壤固碳能力显著增强。而农田和裸地因外源碳投入少, 有机碳含量均是微团聚体>大团聚体>粉黏粒, SOC主要分布在微团聚体中。不同植被覆盖处理对土壤团聚体内密度组分和腐殖质各组分碳的富集“分馏”作用很明显, 与农田和裸地相比, 长期草地植被覆盖处理>2 mm和2-0.25 mm粒级团聚体中轻组碳含量富集的较多, 2-0.25 mm粒级团聚体中富里酸、胡敏酸和胡敏素的碳富集均最高, 而农田和裸地促进了微团聚体内腐殖质碳的富集。草地覆盖显著增加了大团聚体内活性有机碳组分, 来源于植物的碳首先进入到大粒径的团聚体中, 使土壤团聚结构显著改善, 农田和无植被覆盖的裸地土壤中轻组碳含量显著降低, 团聚体内有机碳以重组碳和胡敏素为主, 稳定化程度更高。     

Effects of waterlogging and increased soil nutrients on growth and reproduction of Polygonum hydropiper in the hydro-fluctuation belt of the Three Gorges Reservoir Region

水淹和土壤养分是影响三峡库区消落带植物生长的主要环境因子。消落带不同高程的植物长期经历不同的淹水强度和土壤养分条件。该研究假设同一物种来自于消落带不同高程的植株可能产生性状分化, 从而对根部淹水和土壤养分变化具有不同的生长和繁殖响应策略。为了验证以上假设, 选取在三峡库区消落带高低高程均广泛分布的物种水蓼(Polygonum hydropiper)为研究对象, 采集自然种群的种子。在温室同质园条件下, 研究了根部水淹和土壤养分提升对高低高程水蓼植株生长和繁殖特性的影响。研究结果表明根部水淹显著或趋于显著降低了水蓼植株功能叶的叶长、叶宽、总分枝数、叶生物量、花生物量和总生物量; 低养分处理显著或趋于显著降低了水蓼植株的总节数、总分枝数、根生物量、花生物量和总生物量, 表明根部水淹和低土壤养分对水蓼的生长和繁殖能力具有抑制作用。同时, 根部水淹和土壤养分的交互作用显著影响植株的根生物量, 表明根部水淹条件下高土壤养分更有利于植株根生物量的积累。高高程植株的根生物量和叶生物量显著或趋于显著高于低高程植株, 而低高程植株的始花时间早于高高程植株, 且繁殖分配也显著高于高高程植株, 表明高低高程水蓼植株对资源的分配策略不同。该研究结果表明水蓼的生长和繁殖特性受根部水淹和土壤养分共同限制, 但对根部水淹条件下高土壤养分生境具有较好的适应性; 同时, 低高程植株可以通过调整其生长和繁殖特性以提高对所处生境胁迫的适应性。     

Responses of soil extracellular enzyme activities to carbon input alteration and warming in a subtropical evergreen broad-leaved forest

土壤胞外酶来源于土壤微生物、植物和动物, 是土壤生物地球化学过程的积极参与者, 在森林生态系统的物质循环和能量流动过程中扮演着重要角色。为探明土壤胞外酶活性对碳输入变化及增温的响应, 该研究基于长期增温、去除地表凋落物(以下简称去凋)和切根处理的云南哀牢山亚热带常绿阔叶林控制实验平台, 研究了不同处理(对照、去凋、切根、切根并增温)下表层矿质土壤(0-5和5-10 cm)与碳氮磷获取相关的胞外酶活性, 包括多酚氧化酶(POX)、过氧化物酶(PER)、β-葡萄糖苷酶(BG)、β-1,4-N-乙酰氨基葡萄糖苷酶(NAG)和酸性磷酸酶(AP)。结合铵态氮(NH₄⁺-N)含量、硝态氮(NO₃^--N)含量、溶解有机碳(DOC)含量、溶解总氮(DN)含量、土壤含水量(SWC)等相关指标, 探讨凋落物碳输入、根系碳输入和温度变化对土壤胞外酶活性及其生态化学计量特征的影响。研究结果表明: 在对照样方, 除POX外其余酶活性均为0-5 cm层显著高于5-10 cm层。与对照相比, 长期的凋落物去除显著降低了0-5 cm层土壤AP和BG活性, 对NAG、PER和POX活性则无显著影响; 长期切根处理显著降低了0-5 cm层土壤BG活性, 但提高了两个土层PER活性; 长期切根并增温处理显著降低了0-5 cm层AP和BG活性, 对其余酶活性无显著影响。冗余分析结果显示SWC和NH₄⁺-N含量是驱动土壤酶活性变化的重要因子。本研究为该生态系统土壤碳氮磷生物地球化学关键过程对全球变化的响应提供了土壤酶学的依据。     

Responses of soil respiration to reduced water table and nitrogen addition in an alpine wetland on the Qinghai-Xizang Plateau

近20年来, 青藏高原高寒湿地经历了明显的气候变化, 从而导致多数湿地水位下降和氮沉降的增加。对于湿地生态系统来说, 水位下降意味着土壤通气性能的改善, 可能会导致土壤呼吸的增加; 而氮沉降的增加可能会降低土壤微生物生物量和pH值, 从而可能抑制土壤呼吸。为此, 在青海海北高寒草地生态系统国家野外科学观测研究站利用中宇宙(Mesocosm)实验方法, 探讨了青藏高原高寒泥炭型湿地土壤呼吸对水位降低和氮添加的响应。结果表明: (1)水位降低显著增强了土壤呼吸, 而氮添加对土壤呼吸的影响依赖于水位的变化: 对照水位下, 氮添加显著抑制土壤呼吸; 而水位降低时, 氮添加对土壤呼吸速率无显著影响。(2)土壤呼吸速率与地上生物量、枯落物累积量之间呈显著正相关关系, 而与根系生物量无显著相关关系。(3)水位降低显著提高了土壤呼吸的温度敏感性, 而氮添加对其无显著的影响。因此预测: 随着氮沉降的升高, 高寒泥炭湿地土壤CO₂的排放量将会减少; 然而随着暖干化背景下水位的降低, 青藏高原高寒湿地会排放更多的CO₂。     

Main factors driving changes in soil respiration under altering precipitation regimes and the controlling processes

Aims Our objective was to determine the effects of changes in global pattern of precipitation on soil respiration and the controlling factors. Methods Data were collected from literature on precipitation manipulation experiments globally and a meta-analysis was conducted to synthesize the responses of soil respiration to changes in precipitation regimes. Important findings We found that an increased precipitation stimulated soil respiration while a decreased precipitation suppressed it. When changes in rainfall were normalized to the average treatment level (41% of the current annual precipitation), the level of increases in soil respiration with increased precipitation (49%) were higher than that of decreases with decreased precipitation (21%), showing an asymmetric responses of soil respiration to increases and decreases in precipitation. Soil moisture occurred as the most predominant factor driving the changes in soil respiration under altered precipitation. Changes in soil moisture affected soil respiration directly and indiscreetly by changing aboveground/belowground net primary productivity and microbial biomass carbon, which collectively contributed 98% of variations in soil respiration. In addition, the responses of soil respiration to altered precipitation varied with background temperature and precipitation. The sensitivity of soil respiration increased with local mean annual temperature when precipitation was reduced, while remaining unchanged when precipitation was increased. Meanwhile, the sensitivity of soil respiration to either increases or decreases in precipitation decreased with increasing local mean annual precipitation. Under future altered precipitation regimes, the sensitivity of soil respiration to changes in precipitation is likely dependent of local environment conditions.     

Greenhouse gas fluxes of typical northern subtropical forest soils: Impacts of land use change and reduced precipitation

Aims It is important to study the effects of land use change and reduced precipitation on greenhouse gas fluxes (CO₂, CH₄ and N₂O) of forest soils. Methods The fluxes of CO₂, CH₄ and N₂O and their responses to environmental factors of primary forest soil, secondary forest soil and artificial forest soil under a reduced precipitation regime were explored using the static chamber and gas chromatography methods during the period from January to December in 2014. Important findings Results indicate that CH₄ uptake of primary forest soil ((-44.43 ± 8.73) μg C·m^-2·h^-1) was significantly higher than that of the secondary forest soil ((-21.64 ± 4.86) μg C·m^-2·h^-1) and the artificial forest soil ((-10.52 ± 2.11) μg C·m^-2·h^-1). CH₄ uptake of the secondary forest soil ((-21.64 ± 4.86) μg C·m^-2·h^-1) was significantly higher than that of the artificial forest ((-10.52 ± 2.11) μg C·m^-2·h^-1). CO₂ emissions of the artificial forest soil ((106.53 ± 19.33) μg C·m^-2·h^-1) were significantly higher than that of the primary forest soil ((49.50 ± 8.16) μg C·m^-2·h^-1) and the secondary forest soil ((63.50 ± 5.35) μg C·m^-2·h^-1) (p < 0.01). N₂O emissions of the secondary forest soil ((1.91 ± 1.22) μg N·m^-2·h^-1) were higher than that of the primary forest soil ((1.40 ± 0.28) μg N·m^-2·h^-1) and the artificial forest soil ((1.01 ± 0.86) μg N·m^-2·h^-1). Reduced precipitation (-50%) had a significant inhibitory effect on CH₄ uptake of the artificial forest soil, while it enhanced CO₂ emissions of the primary forest soil and the secondary forest soil. Reduced precipitation had a significant inhibitory effect on CO₂ emissions of the artificial forest soil and N₂O emissions of the secondary forest (p < 0.01). Reduced precipitation promotes N₂O emissions of the primary forest soil and the artificial forest soil. CH₄ uptake of the primary forest and the secondary forest soil increased significantly with the increase of soil temperature under natural and reduced precipitation. CO₂ and N₂O emission fluxes of the primary forest soil, secondary forest soil and artificial forest soil were positively correlated with soil temperature (p < 0.05). Soil moisture inhibited CH₄ uptake of the secondary forest soil and the artificial forest soil (p < 0.05). CO₂ emissions of the primary forest soil were significantly positively correlated with soil moisture (p < 0.05). N₂O emissions of primary forest soil and secondary forest soil were significantly correlated with the nitrate nitrogen content (p < 0.05). It was implied that reduced precipitation and land use change would have significant effects on greenhouse gas emissions of subtropical forest soils.     

土壤碳氮比对平邑甜茶幼苗生长和碳氮分配的影响

为探讨土壤碳氮比(C:N)对苹果(Malus pumila)植株生长和碳氮分配特性的影响, 采用碳氮双标记示踪技术, 以二年生平邑甜茶(Malus hupehensis)幼苗为试验材料, 研究了6个不同土壤C:N处理(T1-T6分别为4.70、9.78、14.70、19.96、25.60和28.83)下平邑甜茶的生长状况和氮素吸收、利用分配以及碳水化合物的运转特性。结果表明, 随着土壤C:N的逐渐增大, 平邑甜茶幼苗根系干重逐渐增加, 而株高、茎粗、地上部干重和植株总干重呈先增加后降低的趋势, 以T4处理最大。土壤C:N显著影响了平邑甜茶幼苗的 ¹⁵N利用率, 从T1到T4处理, 植株的 ¹⁵N利用率逐渐升高, T4处理(18.46%)是T1处理(10.65%)的1.73倍; 随着土壤C:N的进一步增加, 植株的 ¹⁵N利用率逐渐降低, T5和T6处理分别比T4处理降低了1.59%和2.58%。土壤C:N较低的T1和T2处理, 平邑甜茶幼苗各器官从肥料中吸收分配到的 ¹⁵N量对该器官全氮量的贡献率(Ndff)大小顺序为根>叶>茎, 随着土壤C:N的进一步增大, 叶片的Ndff均为最大, 其次是根, 茎最少。随着土壤C:N的增大, 叶片 ¹⁵N分配率逐渐升高, ¹³C分配率逐渐降低; 而根系 ¹⁵N分配率逐渐降低, ¹³C分配率逐渐升高。综合考虑植株生长和氮素利用状况, 本试验条件下适宜平邑甜茶生长的土壤C:N为21-23。     

Effects of storage conditions on total carbon and nitrogen contents of soil and plant samples

Aims The storage of soil and plant samples has important significance for ecological studies, but has not been widely used. This study aims to compare total carbon/nitrogen content of soil and plant samples before and after long term storage, and further to investigate the feasibility of archiving samples for time series ecological studies at large temporal scales.Methods Soil and plant samples were collected in the growing season in 2011. Carbon/nitrogen mass fraction were analyzed after four years of storage, and were compared with the data obtained before storage using pairwise t-test and linear regression.Important findings Nitrogen mass fractions of stored samples were linearly correlated to the data before storage along the 1:1 line under different storage conditions, and the correlation coefficient r was greater than 0.98 (except for soil samples stored at temperature lower than 20 °C and with particle size <2 mm, r = 0.91). The carbon mass fraction after storage was changed by the storage conditions. Carbon mass fractions of stored samples with particle size <0.15 mm were linearly correlated to the data before storage along the 1:1 line (r > 0.98). Carbon mass fractions of samples with particle size <2 mm increased after storage, and the slope of the linear relationship was 1.26 and 1.04 for soil and plant samples respectively. These results indicated that, nitrogen content of stored samples was stable under different storage conditions, while the stability of carbon content was affected by sample particle size but by storage temperature. Archived samples used for carbon/nitrogen analysis were suggested to be ground to particle size <0.15 mm under fully dry and completely sealed conditions.     

Soil water use strategy of dominant species in typical natural and planted shrubs in loess hilly region

Aims Artemisia gmelinii is a dominant specie naturally established after abandonment of cultivated lands in the Loess Plateau, and Caragana korshinskii is one of the main planted shrub species to control soil erosion. Improved understanding of water use strategies of these two species is of great significance to evaluate the sustainable development of the Loess Plateau under the trend of climate warming and increasing drought events.
Methods Stable oxygen-18 isotope was used to determine seasonal variations in the water sources of native A. gmelinii communities established after abandonment of cultivated lands for 7 and 30 years and planted C. korshinskii after 30 years. The contributions of soil water from different depths to water uptake were estimated by the MixSIR Bayesian mixing model. The geometric mean regression method was used to fit the line of precipitation to get the local meteoric water line (LWML).
Important findings The stable hydrogen isotope rate (δD) and stable oxygen isotope rate (δ¹⁸O) of soil water and xylem water plotted to the right side of the LWML, indicating that the isotopic compositions of soil water were enriched due to evaporation. The native A. gmelinii communities established after abandonment of cultivated lands for 7 years and planted C. korshinskii after 30 years showed plasticity in switching water sources from different soil layers, extracting water from shallow soil (0-40 cm) when soil water was available, but deeper soil (40-80 cm) when shallow soil water was dry. In contrast, A. gmelinii growing in site after cultivation abandonment for 30 years mainly relied on water from the surface soil (0-10 cm) throughout the growing season. Our results suggest that the ability of A. gmelinii to compete for soil water reduces with aging of the community while the planted C. korshinskii will have competitive advantage under the condition of increasing frequency of drought events in the future.     

增温对南亚热带森林土壤磷形态的影响及其对有效磷的贡献

磷(P)是森林生态系统生产力的重要限制性元素。土壤磷的有效性取决于磷的存在形态及其转化过程。目前有关增温如何调控磷形态转化过程, 从而促进土壤有效磷含量增加的机制尚未明确。该研究以南亚热带森林为研究对象, 采用沿海拔高度从300 m下降至30 m以模拟温度自然上升的方法, 采集该林型0-10、10-20、20-40 cm的土壤, 并用适用于酸性土壤的连续浸提方法分离不同形态磷, 研究增温对土壤不同形态磷含量的影响, 探讨土壤不同形态磷与有效磷的关系, 识别对土壤有效磷在增温背景下增加有重要贡献的磷组分。结果表明增温使0-10 cm的无机钙磷(Ca-Pi)及20-40 cm的无机铁磷(Fe-Pi)和总无机磷含量分别显著增加了65.5%、17.9%和18.5%, 但对总有机磷及各有机磷组分含量均无显著影响。土壤不同形态磷与有效磷含量的相关分析表明, 有效磷与无机态的不同形态磷及有机铝磷、有机铁磷含量均显著正相关, 其中与Fe-Pi含量的相关性最强。通过土壤不同形态磷与有效磷含量的通径分析进一步发现, 无机铝磷、Fe-Pi是土壤磷转化过程中的重要中间过渡性磷组分, 且Fe-Pi是促进有效磷含量增加最重要的直接贡献磷组分。结合前期研究结果, 增温可能增大了凋落物磷对土壤磷的输入, 还可能强化了土壤的吸附和沉淀过程, 使得更多进入到土壤的溶解态磷转化为Ca-Pi、Fe-Pi等缓效磷源, 其中Fe-Pi可能成为南亚热带森林在气候变暖背景下最重要的有效磷来源。     

Effects of peach branches returning on autotoxins and microbes in soil and tree growth of peaches

Aims This study aimed to investigate the effects of branch returning on the growth of peach (Amygdalus persica "Chunmei/Maotao") saplings, soil enzyme activity, and soil contents of phenolic acids and amygdalin, thereby providing scientific evidence against the application of branch returning for peach trees. Methods One-year-old potted peach tree (Amygdalus persica "Chunmei/Maotao") was used in this study with four agricultural treatments applied, including soil coverage by fragmented peach tree branches (fragment treatment;1.5 and 22.5 g·kg^-1) and applying leachate solutions of peach tree branches to soil (leachate treatment; 1.5 and 22.5 g·kg^-1). No branch addition was used as control (CK). Solid phase extraction, high performance liquid chromatography (HPLC), biological high-throughput sequencing was used to determine the content of autotoxic substances, and microbial community structure in soil. Soil coverage and leachate solution treatments of 30 g and 450 g branches applied to the peach trees were described as 1.5 and 22.5 g·kg^-1, respectively in this paper.Important findings Compared with CK, the phenolic acid and amygdalin contents significantly increased after both fragment and leachate treatments in high quantities (22.5 g·kg^-1). Soil microbial community structure altered in both treatments, with the proportion of fungi (particularly Agaricomycetes, Tubeufia and Cystofilobasidiaceae) increased significantly and bacteria decreased accordingly. Invertase activity in both high-quantity treatments exceeded that in the CK significantly. The activity of catalase and urease was higher at first and then decreased relative to CK under high-quantity fragment and leachate treatments. Specifically, the effect of leachate treatment on enzyme activity was higher than the fragment treatment in the short term. Chlorophyll content, ground diameter (diameter of 5 cm from the ground) growth and net photosynthesis rate of plants were lower in high-quantity fragment and leachate treatments than those in CK, with earlier retardation of new shoot growth. We observed an increase in soil phenolic acids and enzymes in treatments in normal pruning quantity, while no inhibition effect was found on the tree growth. In conclusion, autotoxins (such as phenolic acid and amygdalin) inhibited the growth of peach trees both directly and indirectly through changing soil enzyme activity and microbial community.