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1.
在干旱/半干旱地区,土壤干湿交替是非常普遍的自然现象。近年来,随着极端降水和极端干旱气候事件增加,干湿交替对土壤C和N循环过程影响受到广泛重视。本研究以我国北方半干旱地区科尔沁沙地樟子松人工林为对象,模拟土壤干湿交替对土壤C和N矿化速率影响及其延时效应。结果表明,土壤呼吸CO2释放速率随土壤干旱化增加不断降低,干旱土壤重新湿润后,土壤呼吸速率能够迅速恢复到初始水平。与恒湿处理相比,干湿交替变化能够降低土壤呼吸CO2释放累积量和土壤硝态氮含量;而干湿交替处理土壤呼吸CO2释放累积量、土壤硝态氮含量和净硝化速率均显著高于恒干处理。在干湿交替结束后延时期间,土壤呼吸CO2释放速率、累积释放量对干湿交替变化表现出延时性,而土壤净硝化速率在不同处理间差异不显著。研究表明,土壤水分是影响半干旱地区沙地樟子松人工林土壤C和N循环的重要环境因子,且土壤C和N矿化速率对土壤干湿交替变化的延时响应存在差异。  相似文献   

2.
本研究通过分析开花期灌水对小麦产量、植株养分分配和土壤养分分布的影响及其与根系特性的关系,为小麦充分利用水肥资源提供理论支撑。以抗旱高产品种‘洛麦28'和高光效品种‘百农207'为材料,采用2 m深土柱栽培方法,设置开花期灌水(T1)和开花期不灌水(T2)两个水分处理,测定了不同组织器官、不同土层土壤氮、磷、钾含量及根系分布特性等指标。结果表明: 小麦收获期土壤中铵态氮、速效磷和速效钾主要分布在0~80 cm土层中,硝态氮主要分布在80 cm以下土层中,开花期灌水促进小麦吸收0~60 cm土层的铵态氮、速效磷、速效钾和80 cm以下土层的硝态氮,减少了硝态氮向深层土壤的淋溶;小麦根系主要集中在0~60 cm土层中,随土壤深度的增加而减少。成熟期干物质积累量、全氮和全磷主要分配在小麦籽粒中,而全钾主要分配在茎秆中;开花期灌水显著增加了小麦百粒重,提高了小麦产量;根系形态指标与土壤硝态氮在0~40 cm土层中呈显著负相关,与土壤铵态氮在80~100 cm土层中呈极显著正相关,与土壤速效磷在0~100 cm土层中呈显著正相关。开花期灌水促进了根系在小麦生育末期对土壤养分的充分吸收,延长了养分从营养器官向生殖器官的转运功能期,使营养器官中的养分充分地转运到籽粒中去,增加小麦粒重,进而提高产量。  相似文献   

3.
杉木人工林土壤可溶性有机质及其与土壤养分的关系   总被引:28,自引:5,他引:23  
王清奎  汪思龙  冯宗炜 《生态学报》2005,25(6):1299-1305
通过在福建省来舟林场对不同栽植代数杉木人工林土壤可溶性有机碳(DOC)和氮(DON)及土壤养分的研究,其结果表明,随着杉木栽植代数的增加林地土壤DOC和DON含量逐渐下降,在0~10cm土层内第3代杉木林土壤DOC和DON含量分别是第1代杉木林的83.9%和87.1%、第2代杉木林的90.6%和96.9%,在10~20cm土层内第3代杉木林土壤DOC和DON含量分别是第1代杉木林的80.2%和81.5%、第2代杉木林的81.8%和90.0%。在不同林地和土层内土壤DOC含量之间的差异性达到了显著或极显著水平,而DON含量之间的差异性不显著。不同栽植代数杉木林土壤养分的变化趋势与DOM一致,随着杉木连栽,土壤养分含量呈下降趋势。在0~10cm土层内第3代杉木林土壤全氮、全钾、铵态氮和速效钾含量分别是第1代杉木林的83.1%、60.4%、68.1%和44.3%,是第2代杉木林的84.6%、68.5%、74.4%和58.7%;在10~20cm土层内第3代杉木林土壤全氮、全钾、铵态氮和速效钾含量分别是第1代杉木林的74.0%、53.4%、57.6%和54.6%,是第2代杉木林的94.8%、59.5%、74.3%和65.5%。经相关性分析,在各土层内土壤DOC和DON含量与土壤全氮、全钾、铵态氮和速效钾等土壤养分含量存在着不同程度的相关性。  相似文献   

4.
通过室内恒湿和干湿交替培养试验,研究了沈阳地区耕地棕壤和草甸土的固钾特征,及其施用有机肥后对土壤固钾作用的影响。结果表明,在保持土壤处于田间持水量的恒湿条件下,两种土壤对外源钾都能够产生快速固定作用,经过1d培养土壤的固钾作用就可以达到平衡,但干湿交替培养可以提高土壤固钾量26.80%~33.27%;土壤施用有机肥后,在恒湿和干湿交替培养条件下均可以降低土壤的固钾强度,其中,施用有机肥6%处理的恒湿培养15d后,棕壤和草甸土的固钾量分别降低了25.71%和36.62%。  相似文献   

5.
田间试验条件下,以转双价(Bt+CpTI)基因棉SGK321及其非转基因亲本常规棉石远321为研究对象,比较分析不同生育期(30、60、90、120d)转双价基因棉和亲本棉根际土壤酶活性(脲酶、碱性磷酸酶、过氧化氢酶)及速效养分(硝态氮、铵态氮和速效磷)的变化。结果表明,转双价基因棉根际土壤硝态氮、铵态氮和速效磷含量变化趋势与其亲本常规棉基本一致,但各养分的具体变化幅度因生育期不同而异。播种后30、60、120d转双价基因棉和亲本常规棉根际土壤碱性磷酸酶活性无显著差异;土壤脲酶和过氧化氢酶活性随棉花生育进程其变化趋势虽各不相同,但同一生育期转双价基因棉与亲本常规棉根际土壤脲酶和过氧化氢酶活性均无显著差异。表明,土壤酶活性和速效养分含量受转双价基因棉的影响较小,其变化主要受生育期的影响。  相似文献   

6.
干湿交替频率对不同土壤CO2和N2O释放的影响   总被引:4,自引:0,他引:4  
欧阳扬  李叙勇 《生态学报》2013,33(4):1251-1259
干旱、半干旱和地中海气候区,乃至一些湿润地区,由干湿交替引起的土壤碳、氮的短暂脉冲式释放很大程度上决定着长时间尺度温室气体释放的总量,是土壤碳、氮温室气体释放的关键过程.选择我国降雨梯度下的森林、农田、草地和荒漠生态系统,采集土样进行实验室统一控制条件下的多重干湿交替循环,对比探讨不同生态系统土壤干湿交替频率对CO2和N2O释放的影响模式.结果表明:(1)干湿交替能够显著的激发土壤中CO2和N2O的释放,森林、农田、草地和荒漠土壤CO2和N2O释放速率对干湿交替的响应模式基本一致,其响应强度与土壤本底中碳和氮的含量有关;(2)在一定培养时间内,随着干湿交替频率的增加,土壤再湿润阶段CO2释放速率降低,但是,气体释放的总量较之于恒湿对照组有所增加.(3)不同土壤N2O的释放总量对于湿交替频率的响应模式表现出很大的差异,其中农田和荒漠土壤响应模式类似.  相似文献   

7.
菜地和一般农田土壤主要养分累积的差异   总被引:59,自引:10,他引:49  
选取不同类型菜地和一般农田 ,测定了 0~ 2 0 0cm土壤剖面的有机质、全氮、硝态氮、铵态氮、速效磷、速效钾等主要养分含量及其分布 .结果表明 ,菜地土壤中养分大量累积 ,其中硝态氮和速效磷累积程度较高 .大棚和露天菜地 0~ 2 0 0cm土层的硝态氮累积总量分别为 15 2 0 .9kg·hm-2 和 135 8.8kg·hm-2 ,比农田高出 5 .2和 4.5倍 ;速效磷分别为 978.1kg·hm-2 和 5 0 3.3kg·hm-2 ,比农田高出 6 .2和 2 .7倍 .而其它养分增加相对较少 .有机质累积总量分别为 2 80 .5Mg·hm-2 和 2 6 9.3Mg·hm-2 ,比一般农田高出 12 .5 %和 8.0 % ;全氮分别为 37.5Mg·hm-2 和 32 .7Mg·hm-2 ,比农田高出 36 .2 %和 18.6 % ;铵态氮分别为 2 11.5kg·hm-2 和 197.8kg·hm-2 ,比农田高出 2 9.6 %和 2 1.2 % ;速效钾分别为 6 5 6 7.8kg·hm-2 和 5 5 2 3 .6kg·hm-2 ,比农田高出 30 .6 %和 9.8% .此外 ,菜地土壤中累积的养分不仅分布在表层 ,在深层土壤也大量存在 ,说明菜地存在严重的养分淋溶现象 .  相似文献   

8.
干湿交替(DW)对土壤有机碳矿化作用、养分循环和微生物生长代谢有着重要的影响。本文选择武夷山不同海拔0~10 cm的表层土壤作为研究对象,分别在5、15和25℃温度下培养,模拟DW循环,并设置恒湿处理(CW)作为对照,研究干湿循环对不同海拔土壤碳矿化作用的影响。结果表明:与CW处理相比,土壤变干时显著减少土壤有机碳矿化速率。重新变湿后,土壤有机碳的脉冲效应被观察,且变湿的脉冲效应随着DW数的增加而逐渐降低。重复的DW处理土壤累积碳矿化量显著低于CW处理,表明湿润引起的激发碳矿化量不足以抵消干旱期间减少量。DW处理的温度敏感性Q10显著低于CW处理。在DW循环中,湿度敏感性k值随海拔的升高而增加,表明高海拔土壤矿化更强的水分依赖性。DW处理微生物生物量碳含量高于CW处理,而冷水和热水浸提的可溶性有机碳含量则低于CW处理。  相似文献   

9.
通过2018年早稻和晚稻田间试验,研究化学氮肥减量及配施稻秆生物炭对稻田土壤养分特性及植株氮素吸收的影响。试验包括6个处理:不施氮(CK)、常规施氮(N100)、减氮20%(N80)、减氮20%配施生物炭(N80+BC)、减氮40%(N60)、减氮40%配施生物炭(N60+BC)。结果表明: 与常规施氮相比,单纯减氮20%和40%或配施生物炭对早晚稻不同生育期土壤pH、有机质、全氮、铵态氮、全磷、有效磷、全钾、速效钾无显著影响;减氮20%配施生物炭显著增加晚稻分蘖期的土壤阳离子交换量(CEC),而减氮40%配施生物炭则显著增加晚稻抽穗期的电导率(EC)值。与单纯减氮相比,N80+BC的土壤速效钾含量在早晚稻抽穗期均显著升高,土壤pH值、全氮在晚稻成熟期显著增加;N60+BC的土壤全钾含量在早稻成熟期显著升高。不同处理早稻土壤硝态氮含量随生育进程逐渐降低,与分蘖期相比,抽穗期和成熟期的常规施氮土壤硝态氮含量分别降低50.0%和71.6%,而配施生物炭处理则降低6.3%~45.5%,减氮配施生物炭显著降低了硝态氮的流失。在晚稻抽穗期,减氮配施生物炭植株吸氮量显著高于常规施氮和单纯减氮,增加幅度为34.8%~52.4%。综上,适度的减氮或配施稻秆生物炭能有效保持土壤养分,促进水稻对氮素的吸收,提高氮素利用率。  相似文献   

10.
放牧制度对荒漠草原生态系统土壤养分状况的影响   总被引:4,自引:1,他引:3       下载免费PDF全文
从土壤N,P,K及土壤有机质等方面研究了在连续进行了7 a的放牧制度试验对荒漠草原生态系统土壤养分含量的影响。研究结果表明:放牧制度对土壤的养分状况有明显的影响。划区轮牧区和禁牧提高了土壤有机质、土壤氮素、土壤全钾和土壤速效钾含量。土壤表层磷含量划区轮牧区最高。放牧导致碳氮比减少。同时,土壤养分含量随土壤深度的变化在不同处理没有表现出较为一致的变化趋势。禁牧区土壤全氮含量随土壤深度的增加而增加;不同处理土壤速效氮、土壤速效钾含量均随土壤深度的增加逐渐降低;土壤全磷在自由放牧区随土壤深度的增加逐渐升高;土壤速效磷、全钾含量在划区轮牧区随土壤深度的增加逐渐降低;土壤养分含量与土壤深度的拟合曲线为二次幂函数。研究表明,禁牧和划区轮牧较自由放牧可以提高荒漠草原土壤养分元素的含量,有利于遏制草原土壤的退化。  相似文献   

11.
在干旱/半干旱地区,土壤干湿交替现象非常明显.在全球气候变化背景下,预测未来科尔沁沙地的土壤干湿交替变化强度将进一步加剧.本研究采用室内原位土柱培养方法,模拟干湿交替对科尔沁沙地小叶杨和樟子松叶凋落物分解速率及养分释放的影响.试验设置3个处理:恒湿处理(CM)、轻度干湿交替处理(DW1,10 d干燥+20 d湿润)和重度干湿交替处理(DW2,20 d干燥+10 d湿润).整个培养试验共处理180 d,其中进行4次干湿交替循环处理,并在干湿交替处理结束后,将各处理置于相同土壤水分条件(60%田间持水量)延时培养60 d.结果表明: 小叶杨和樟子松叶凋落物分解及养分释放对干湿交替的响应一致.在干湿交替期间,DW2处理显著抑制叶凋落物分解及叶凋落物C、木质素和总酚释放;与CM相比,DW2处理叶凋落物质量、C、木质素和总酚残留率分别增加17.4%、23.8%、35.2%和32.7%,而干湿交替对叶凋落物N和P养分释放无显著影响.干湿交替处理结束和延时培养结束时,不同干湿处理叶凋落物分解及养分残留率的变化具有一致性.而延时培养期间DW2处理凋落物分解速率、叶凋落物C和木质素释放加快,表明干湿交替对叶凋落物分解及养分释放具有短期延时效应.  相似文献   

12.
Winter climate change is an important environmental driver that alters the biogeochemical processes of forest soils. The decrease in snowpack amplifies soil freeze–thaw cycles and decreases the snowmelt water supply to soil. This study examined how snow decrease affects nitrogen (N) mineralization and nitrification in forest soil in northern Japan by conducting an in situ experimental snowpack manipulation experiment and a laboratory incubation of soil with different moisture, temperature and freeze–thaw magnitudes. For the incubation studies, surface mineral soil (0–10 cm) was collected from a cool-temperate natural mixed forest and incubated using the resin core method during the winter. In the field, there were two treatments: 50 and 100 % snow removal and control plots. The increase in the soil freeze–thaw cycle increased net N mineralization and marginally decreased the net nitrification in soil. The dissolved organic carbon (DOC) and DOC/DON ratio in soil increased with the decrease in snowpack especially during the snow melt period. These results suggested that the change in substrate quality by the increase in freeze–thaw cycles caused the significant enhancement of microbial ammonium production in soil. The lower soil moisture and higher gross immobilization of inorganic N by soil microbes may be maintaining the slow net nitrification and low nitrate leaching in freeze–thaw cycles with less snowpack. The results indicate that winter climate change would strongly impact N biogeochemistry through the increase in ammonium availability in soil for plants and microbes, whereas it would be unlikely that nitrate loss from surface soil would be enhanced.  相似文献   

13.

Aims

There are few studies on the interactive effect of salinity and sodicity in soils exposed to drying and wetting cycles. We conducted a study to assess the impact of multiple drying and wetting on microbial respiration, dissolved organic carbon and microbial biomass in saline and saline-sodic soils.

Methods

Different levels of salinity (EC1:5 1.0 or 2.5) and sodicity (SAR?<?3 or 20) were induced by adding NaCl and CaCl2 to a non-saline/non-sodic soil. Finely ground wheat straw residue was added at 20?g?kg?1 as substrate to stimulate microbial activity. The constant moist (CM) treatment was kept at optimum moisture content for the length of the experiment. The drying and rewetting (DW) treatments consisted of 1 to 3 DW cycles; each DW cycle consisted of 1?week drying after which they were rewet to optimum moisture and then maintained moist for 1?week.

Results

Drying reduced respiration more strongly at EC2.5 than with EC1.0. Rewetting of dry soils produced a flush in respiration which was greatest in the soils without salt addition and smallest at high salinity (EC2.5) suggesting better substrate utilisation by microbes in soils without added salts. After three DW events, cumulative respiration was significantly increased by DW compared to CM, being 24% higher at EC1.0 and 16% higher at EC2.5 indicating that high respiration rates after rewetting may compensate for the low respiration rates during the dry phase. The respiration rate per unit MBC was lower at EC2.5 than at EC1.0. Further, the size of the flush in respiration upon rewetting decreased with each ensuing DW cycle being 50–70% lower in the third DW cycle than the first.

Conclusions

Both salinity and sodicity alter the effect of drying and rewetting on soil carbon dynamics compared to non-saline soils.  相似文献   

14.
模拟氮沉降对温带典型森林土壤有效氮形态和含量的影响   总被引:4,自引:4,他引:0  
陈立新  段文标 《生态学杂志》2011,22(8):2005-2012
通过室内模拟氮沉降试验,研究了氮沉降对温带典型森林土壤有效氮的影响.结果表明:试验期间,与对照相比,经过氮沉降处理的土壤铵态氮、硝态氮和有效氮均呈增长的趋势,增加的程度取决于森林类型、土层、氮处理类型和氮处理的持续时间.氮沉降对不同林型土壤有效氮形态和含量的影响不同,氮沉降对混交林的影响弱于阔叶林,强于针叶人工纯林;土壤A层对氮沉降的敏感程度大于土壤B层;铵态氮形态沉降对土壤铵态氮含量的影响比对土壤硝态氮含量的影响大,而硝态氮形态沉降对土壤硝态氮含量的影响比对土壤铵态氮含量的影响大,混合形态的氮沉降对二者均有促进作用,且增加幅度更高;氮沉降对土壤有效氮的影响存在累加效应.  相似文献   

15.
Climate change alters frequencies and intensities of soil drying-rewetting and freezing-thawing cycles. These fluctuations affect soil water availability, a crucial driver of soil microbial activity. While these fluctuations are leaving imprints on soil microbiome structures, the question remains if the legacy of one type of weather fluctuation (e.g., drying-rewetting) affects the community response to the other (e.g., freezing-thawing). As both phenomenons give similar water availability fluctuations, we hypothesized that freezing-thawing and drying-rewetting cycles have similar effects on the soil microbiome. We tested this hypothesis by establishing targeted microcosm experiments. We created a legacy by exposing soil samples to a freezing-thawing or drying-rewetting cycle (phase 1), followed by an additional drying-rewetting or freezing-thawing cycle (phase 2). We measured soil respiration and analyzed soil microbiome structures. Across experiments, larger CO2 pulses and changes in microbiome structures were observed after rewetting than thawing. Drying-rewetting legacy affected the microbiome and CO2 emissions upon the following freezing-thawing cycle. Conversely, freezing-thawing legacy did not affect the microbial response to the drying-rewetting cycle. Our results suggest that drying-rewetting cycles have stronger effects on soil microbial communities and CO2 production than freezing-thawing cycles and that this pattern is mediated by sustained changes in soil microbiome structures.Subject terms: Soil microbiology, Biogeochemistry, Biodiversity, Microbial ecology  相似文献   

16.
通过室内培养试验,研究了不同浓度氯嘧磺隆(20、200、2000 μg·kg-1土)单一施用及与尿素(120 mg· kg-1土)配合施用情况下,土壤微生物生物量碳、氮和土壤铵态氮、硝态氮随时间的动态变化规律.结果表明:各浓度氯嘧磺隆单独处理在整个培养期(60 d)中对微生物生物量碳、氮均有抑制作用,且浓度越高,后期抑制作用越强;各浓度氯嘧磺隆处理在培养前期对硝态氮、铵态氮没有明显影响,中期(15 d)能显著提高土壤中铵态氮的含量,后期(30 d后)显著提高了土壤中硝态氮的含量.尿素单独施用及与氯嘧磺隆配施均能在短时间内增加微生物生物量碳、氮,但随后配施处理的促进作用减弱;尿素单独和配施均能持久增加土壤中铵态氮、硝态氮含量.  相似文献   

17.
The ongoing climate change is predicted to induce more weather extremes such as frequent drought and high-intensity precipitation events, causing more severe drying-rewetting cycles in soil. However, it remains largely unknown how these changes will affect soil nitrogen (N)-cycling microbes and the emissions of potent greenhouse gas nitrous oxide (N2O). Utilizing a field precipitation manipulation in a semi-arid grassland on the Loess Plateau, we examined how precipitation reduction (ca. −30%) influenced soil N2O and carbon dioxide (CO2) emissions in field, and in a complementary lab-incubation with simulated drying-rewetting cycles. Results obtained showed that precipitation reduction stimulated plant root turnover and N-cycling processes, enhancing soil N2O and CO2 emissions in field, particularly after each rainfall event. Also, high-resolution isotopic analyses revealed that field soil N2O emissions primarily originated from nitrification process. The incubation experiment further showed that in field soils under precipitation reduction, drying-rewetting stimulated N mineralization and ammonia-oxidizing bacteria in favor of genera Nitrosospira and Nitrosovibrio, increasing nitrification and N2O emissions. These findings suggest that moderate precipitation reduction, accompanied with changes in drying-rewetting cycles under future precipitation scenarios, may enhance N cycling processes and soil N2O emissions in semi-arid ecosystems, feeding positively back to the ongoing climate change.  相似文献   

18.
土壤活性有机质及其与土壤质量的关系   总被引:86,自引:2,他引:86  
活性有机质是土壤的重要组成部分 ,主要包括溶解性有机碳、微生物生物量、轻组有机质。它在土壤中具有重要作用 :(1)可以表征土壤物质循环特征、评价土壤质量 ,可以作为土壤潜在生产力以及由土壤管理措施引起土壤有机质变化的早期指标 ;(2 )在养分周转中起重要作用 ,是植物的养分库 ,可以提供植物所需要的养分如氮、磷、硫等 ;(3)能稳定土壤结构 ,对维持团粒结构稳定性有重要作用。从土壤养分、土壤物理、化学性质方面讨论了活性有机质与土壤质量的关系。土壤中的溶解性有机碳、微生物生物量碳氮含量与土壤有机碳、全氮和碱解氮等物质的含量呈正相关。活性有机质受土壤质地、含水量、温度等因素影响 ,与土壤酸碱度、阳离子交换量等也有关。土壤微生物生物量碳和微生物量 C/有机碳比与土壤粘粒、粉粒含量呈正相关、与砂粒含量呈负相关  相似文献   

19.
Rhizosphere microbial community is important for the acquisition of soil nutrients and closely related to plant species. Fertilisation practice changed soil quality. With the hypothesis of stronger rhizosphere effect of plant on rhizosphere microbial community than fertilisation management, we designed this research based on a long‐term field experiment (1982–present). This study consists of no fertilisation (NF), mineral fertilisers (NPK), mineral fertilisers plus 7,500 kg/ha of wheat straw addition (WS) and mineral fertilisers plus 30,000 kg/ha of cow manure (CM). After analysing, we found that fertilisation management not only elevated crop yield but also affected crop rhizosphere microbial community structure. The influence of fertilisation practice on wheat rhizosphere microbial structure was stronger than that of wheat. For wheat rhizosphere bacterial community, it was significantly affected by soil water content (SWC), nitrogen (TN), phosphorus (TP), pH, available phosphorus (AVP) and nitrogen (AVN), dissolved organic nitrogen (DON) and carbon (DOC). Besides SWC, pH, AVP, AVN, TN, TP and DOC, the wheat rhizosphere fungi community was also significantly affected by soil organic matter (SOM) and available potassium (AVK). Moreover, compared to rhizosphere bacterial community, the influences of soil physiochemical properties on rhizosphere fungal community was stronger. In conclusion, fertilisation practice was the primary factor structuring rhizosphere microbial community by changing soil nutrients availabilities in the agroecosystem.  相似文献   

20.
在2010年5月—2011年4月和2011年5月—2012年4月2个培养周期内,采用原状土柱野外控制试验,利用海拔梯度变化研究了温度增加对川西高山森林土壤溶解性有机碳(DOC)和有机氮(DON)动态的影响.结果表明: 经模拟增温处理(降低海拔)的土壤有机层和矿质土壤层DOC和DON含量在2个连续培养周期内的各关键时期均呈现明显的动态变化.海拔3300和3000 m样地比海拔3600 m 样地土层DOC含量分别增加6.8和26.6 mg·kg-1.海拔3600、3300和3000 m样地土层DOC含量均在第1个培养周期的生长季末最高,分别为408.0、317.9和448.2 mg·kg-1,在第2个培养周期的生长季节中期最低, 分别为33.1、32.4和36.5 mg·kg-1.与海拔3600 m样地相比,海拔3300和3000 m样地土层DON含量分别增加2.3和30.4 mg·kg-1.除海拔3000 m样地以外,海拔3600和3300 m样地土层DON含量在第1个培养周期内的生长季节中期最高,分别为65.9和64.6 mg·kg-1,在第1个培养周期内的融化期最低,分别为31.9和37.1 mg·kg-1.模拟增温处理增加了样地内土壤有机层DOC和DON含量,降低了矿质土壤层DOC含量、土壤有机层及矿质土壤层DOC/DON值.土壤有机层DOC/DON值与DOC含量呈显著正相关,与DON含量呈显著负相关;矿质土壤层DOC/DON值与DOC含量呈显著负相关,与DON含量呈显著正相关.未来全球气候变暖可能通过影响高寒森林土壤温度和冻融循环格局,增加整个土层DOC和DON含量,进而影响高寒森林土壤碳、氮循环过程.  相似文献   

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