灌淤土农田土壤有机碳及碳库管理指数对施肥措施的响应

为了探讨施肥对灌淤土水旱轮作农田土壤有机碳和碳库管理指数的影响特征,寻求合适的土壤增碳措施,在宁夏引黄灌区水稻-春小麦-春玉米轮作体系中,通过3 a田间定位试验研究了不施肥(CK)、平衡施用化肥(NPK)、单施有机肥(M)、化肥+有机肥配施(NPK+M)、化肥+玉米秸秆(NPK+S)和农民习惯施肥(CON)6个不同施肥措施对0~20 cm耕层土壤总有机碳、活性有机碳含量及碳库管理指数的影响。结果表明,在同等氮素供应水平下,无论水田或旱地,NPK、M、NPK+M和NPK+S处理都能达到土壤增碳效果,3年的土壤培肥后,其土壤总有机碳和活性有机碳含量分别达10.03~10.60 g·kg~(-1)和3.00~4.35 g·kg~(-1),与试验前(9.92 g·kg~(-1)和2.48g·kg~(-1))相比分别提高了1.2%~6.8%和20.8%~75.2%,M处理显著高于CK。施用有机肥3 a以上,才能显著提高土壤碳库、碳库活度、活度指数和碳库管理指数。因此,从土壤总有机碳及其活性组分提升的角度考虑,应在平衡施用NPK的基础上,提倡水旱轮作农田长期增施有机肥来提高土壤碳库管理指数。     

黄土高原子午岭油松林管理方式对黑碳和颗粒有机碳积累的影响

对黄土高原子午岭油松林不同管理方式下土壤的黑碳(BC)、有机碳(POC)和活性有机碳(LOC)的空间分布和积累进行了研究.结果表明,各种管理方式的油松林其POC、LOC和BC由表层至下层均呈显著的降低规律性.各种管理方式油松林0～10cm土层以BC>POC>LOC,10～20 cm土层中,天然油松林和粗放管理型油松林B...     

The impact of land use change on soil organic carbon and labile organic carbon stocks in the Longzhong region of Loess Plateau

Land use change (LUC) is widely recognized as one of the most important driving forces of global carbon cycles. The soil organic carbon (SOC) and labile organic carbon (LOC) stores were investigated at arable land (AL), artificial grassland (AG), artificial woodland (AW), abandoned arable land (AAL) and desert steppe (DS) in the Longzhong region of the Loess Plateau in Northwest China. The results showed that conversions from DS to AL, AL to AG and AL to AAL led to an increase in SOC content, while the conversion from DS to AW led to a decline. The differences in SOC content were significant between DS and AW at the 20-40 cm depth and between AL and AG at the 0-10 cm depth. The SOC stock in DS at the 0-100 cm depth was 39.4 t/hm 2 , increased by 28.48% after cultivation and decreased by 19.12% after conversion to AW. The SOC stocks increased by 2.11% from AL to AG and 5.10% from AL to AAL. The LOC stocks changed by a larger magnitude than the SOC stocks, which suggests that it is a more sensitive index of carbon dynamics under a short-term LUC. The LOC stocks increased at 0-20 cm and 0-100 cm depths from DS to AW, which is opposite to that observed for SOC. The proportion of LOC to SOC ranged from 0.14 to 0.20 at the 0-20 cm depth for all the five land use types, indicating low SOC dynamics. The allocation proportion of LOC increased for four types of LUC conversion, and the change in magnitude was largest for DS to AW (40.91%). The afforestation, abandonment and forage planting on arable land led to sequestration of SOC; the carbon was lost initially after afforestation. However, the carbon sink effect after abandonment may not be sustainable in the study area.     

山西太岳山不同林分土壤有机碳储量研究

基于山西太岳山系灵空山景区侧柏林、油松林、辽东栎林、辽东栎和油松混交林4种林分调查,通过密集采样和样品分析研究不同林分土壤不同层次(0-10cm、10-20cm、20-30cm、30-50cm、50-100cm)有机碳含量、有机碳密度和有机碳储量及分布特征。结果如下:山西太岳山森林平均1m土层土壤的有机碳储量一般不超过30g·kg-1,调查的四种林分在16.2g·kg-1到29.6g·kg-1;所调查的四种林分的土壤有机碳储量、碳密度随着土层深度递减,其中油松林、侧柏林、辽东栎林30cm以上土壤中有机碳储量占到100cm土层中有机碳储量的85%以上,表层土壤碳储量贡献大;阔叶林碳储量高于针叶林,混交林碳储量高于纯林,辽东栎油松针阔混交林土壤有机碳含量是油松林土壤碳含量的2.4倍,辽东栎林土壤碳储量大约分别是侧柏林、油松林的1.4和1.9倍。因此为增加森林土壤固碳,建议使用混交林并减少人类活动对森林表土层的干扰和破坏。     

不同耕作措施下陇中黄土高原旱作农田土壤活性有机碳组分及其与酶活性间的关系

通过设置在陇中黄土高原半干旱雨养农业区15年的不同保护性耕作措施长期定位试验,研究了传统耕作(T)、免耕(NT)、免耕结合秸秆覆盖(NTS)、传统耕作结合秸秆还田(TS)4种不同耕作措施下不同土层的土壤总有机碳、土壤活性有机碳、土壤微生物量、碳库管理指数和土壤蔗糖酶、淀粉酶、纤维素酶和过氧化物酶等4种参与碳循环土壤酶,并分析了土壤有机碳及其活性碳组分与土壤酶之间的相关关系。结果表明:0~30 cm土层,NTS处理可显著提高土壤有机碳、土壤活性有机碳、土壤微生物量碳及碳库管理指数,分别较T处理增加了16.3%、28.26%、41.88%、37.04%,NT、TS处理较T处理各指标也均有不同程度提高;在0~30 cm土层,NTS、TS、NT处理与T处理相比,蔗糖酶分别提高了33.84%、21.59%、25.15%,淀粉酶活性分别提高了20.90%、13.43%、12.69%,纤维素酶活性分别提高了39.13%、17.39%、4.34%,过氧化物酶活性分别提高了7.81%、2.08%、3.65%;土壤蔗糖酶、淀粉酶、纤维素酶、过氧化物酶与各形态有机碳及碳库管理指数均表现为显著或极显著正相关关系;蔗糖酶活性增加对有机碳积累作用最显著,有助于土壤总有机碳、活性有机碳、微生物量碳含量提高,土壤纤维素酶对土壤总有机碳和活性有机碳含量的增加有促进作用,过氧化物酶有利于总有机碳的积累。免耕结合秸秆覆盖是适宜该地区农田生态系统健康稳定发展,减少碳库损失的重要途径。     

连续14年保护性耕作对土壤总有机碳和轻组有机碳的影响

依托于2001年布设在陇中黄土高原半干旱雨养农业区的保护性耕作定位试验,于2014年测定了5种保护性耕作(免耕+秸秆覆盖NTS、免耕NT、传统耕作+秸秆翻埋TS、传统耕作+地膜覆盖TP和免耕+地膜覆盖NTP)和传统耕作T处理下小麦-豌豆双序列轮作中表层土壤(0~5、5~10、10~30 cm)总有机碳(SOC)和轻组有机碳(LFOC)在作物生育期前后的变化。结果表明:土壤总有机碳和轻组有机碳在土壤剖面上均随着土层深度的增加而降低;相比传统耕作T,NTS和TS处理能显著提高0~30 cm土层中SOC、LFOC的含量,在作物播种前较T分别提高了19.51%、64.58%和13.36%、42.08%,在收获后分别提高了28.00%、85.37%和18.61%、77.82%,而SOC、LFOC含量NT和TP处理与T处理间差异不显著;从作物播种前至收获后,各处理下0~30 cm土层SOC含量均有减小趋势,其中NTS和TS处理变化量最小,NT和TP处理加大了作物生育期间SOC和LFOC的消耗;LFOC可以灵敏地反应出土壤有机碳的变化。因此,在该区推行以免耕、秸秆覆盖为主的保护性耕作措施更有利于碳的积累和土壤质量的改善,促进该区农业的可持续发展。     

Impact of rainfed and irrigated agriculture systems on soil carbon stock under different climate scenarios in the semi-arid region of Brazil

Understanding the dynamics of soil organic carbon (SOC) is of fundamental importance in land use and management, whether in the current researches or in future scenarios of agriculture systems considering climate change. In order to evaluate SOC stock of the three districts (Delmiro Gouveia, Pariconha, and Inhapi districts) in the semi-arid region of Brazil in rainfed and irrigated agriculture systems under different climate scenarios using the Century model, we obtained RCP4.5 and RCP8.5 climate scenarios derived from the Eta Regional Climate Model (Eta-HadGEM2-ES and Eta-MIROC5) from the National Institute for Space Research, and then input the data of bulk density, pH, soil texture, maximum temperature, minimum temperature, and rainfall into the soil and climate files of the Century model. The results of this study showed that the Eta-HadGEM2-ES model was effective in estimating air temperature in the future period. In rainfed agriculture system, SOC stock under the baseline scenario was lower than that under RCP4.5 and RCP8.5 climate scenarios, while in irrigated agriculture system, SOC stock in the almost all climate scenarios (RCP4.5 and RCP8.5) and models (Eta-HadGEM2-ES and Eta-MIROC5) will increase by 2100. The results of this study will help producers in the semi-arid region of Brazil adopt specific agriculture systems aimed at mitigating greenhouse gas emissions.     

Decomposition characteristics of organic materials and their effects on labile and recalcitrant organic carbon fractions in a semi-arid soil under plastic mulch and drip irrigation

Labile organic carbon(LC) and recalcitrant organic carbon(RC) are two major fractions of soil organic carbon(SOC) and play a critical role in organic carbon turnover and sequestration. The aims of this study were to evaluate the variations of LC and RC in a semi-arid soil(Inner Mongolia, China) under plastic mulch and drip irrigation after the application of organic materials(OMs), and to explore the effects of OMs from various sources on LC and RC by probing the decomposition characteristics of OMs using in-situ nylon mesh bags burying method. The field experiment included seven treatments, i.e., chicken manure(CM), sheep manure(SM), mushroom residue(MR), maize straw(MS), fodder grass(FG), tree leaves(TL) and no OMs as a control(CK). Soil LC and RC were separated by Huygens D's method(particle size-density), and the average soil mass recovery rate and carbon recovery rate were above 95%, which indicated this method was suitable for carbon pools size analysis. The LC and RC contents significantly(P0.01) increased after the application of OMs. Moreover, LC and RC contents were 3.2%–8.6% and 5.0%–9.4% higher in 2016 than in 2015. The applications of CM and SM significantly increased(P0.01) LC content and LC/SOC ratio, whereas they were the lowest after the application of TL. However, SOC and RC contents were significantly higher(P0.01) after the applications of TL and MS. The correlation analysis indicated the decomposition rate of OMs was positively related with LC content and LC/SOC ratio. In addition, lignin, polyphenol, WOM(total water-soluble organic matter), WHA(water-soluble humic acid), HSL(humic-like substance) and HAL(humic acid-like) contents in initial OMs played important roles in SOC and RC. In-situ nylon mesh bags burying experiment indicated the decomposition rates of CM, SM and MS were significantly higher than those of MR, FG, and TL. Furthermore, MS could result in more lignin derivatives, WHA, and HAL polymers in shorter time during the decomposition process. In conclusion, the application of MS in the semi-arid soil under a long-term plastic mulch and drip irrigation condition could not only improve soil fertility, but also enhance soil carbon sequestration.     

Corn straw return can increase labile soil organic carbon fractions and improve water-stable aggregates in Haplic Cambisol

Corn straw return to the field is a vital agronomic practice for increasing soil organic carbon (SOC) and its labile fractions, as well as soil aggregates and organic carbon (OC) associated with water-stable aggregates (WSA). Moreover, the labile SOC fractions play an important role in OC turnover and sequestration. The aims of this study were to determine how different corn straw returning modes affect the contents of labile SOC fractions and OC associated with WSA. Corn straw was returned in the following depths: (1) on undisturbed soil surface (NTS), (2) in the 0-10 cm soil depth (MTS), (3) in the 0-20 cm soil depth (CTS), and (4) no corn straw applied (CK). After five years (2014-2018), soil was sampled in the 0-20 and 20-40 cm depths to measure the water-extractable organic C (WEOC), permanganate oxidizable C (KMnO₄-C), light fraction organic C (LFOC), and WSA fractions. The results showed that compared with CK, corn straw amended soils (NTS, MTS and CTS) increased SOC content by 11.55%-16.58%, WEOC by 41.38%-51.42%, KMnO₄-C and LFOC by 29.84%-34.09% and 56.68%-65.36% in the 0-40 cm soil depth. The LFOC and KMnO₄-C were proved to be the most sensitive fractions to different corn straw returning modes. Compared with CK, soils amended with corn straw increased mean weight diameter by 24.24%-40.48% in the 0-20 cm soil depth. The NTS and MTS preserved more than 60.00% of OC in macro-aggregates compared with CK. No significant difference was found in corn yield across all corn straw returning modes throughout the study period, indicating that adoption of NTS and MTS would increase SOC content and improve soil structure, and would not decline crop production.     

退耕年限与方式对土壤团聚体稳定性及有机碳分布的影响

以黄土高原南部退耕还林年限6 a(FL06)和15 a(FL15)刺槐林地、退耕还草年限6 a(GL06)和15 a(GL15)紫花苜蓿草地为研究对象,以临近长期耕作坡耕地(CK)作为对照,采用湿筛法,分离出2 mm、1~2 mm、0.5~1 mm、0.25~0.5 mm和0.25 mm 5个粒级的水稳性团聚体,研究了退耕年限与方式对团聚体稳定性和不同粒径团聚体有机碳分布的影响。结果表明:在0~20 cm土层,退耕还林还草与未退耕相比能显著提高2 mm和1~2 mm粒径团聚体含量,显著减少0.25 mm粒径团聚体含量,其中对于2 mm和1~2 mm粒径团聚体在不同退耕年限与方式下含量表现为GL15GL06FL06FL15CK和GL15FL06GL06FL15CK;退耕还林和还草增加了两个土层的团聚体稳定性,GL15的平均重量直径(MWD)值和几何平均直径(GMD)值均最大,土壤结构最稳定,其次为GL06;不同退耕年限,2 mm粒径下退耕还林地和还草地、1~2 mm粒径下退耕还草地团聚体有机碳含量均随退耕年限的延长而增加。20~40 cm土层中,团聚体含量均值随粒径的减小而增加;MWD和GMD值均小于0~20 cm层;各粒径范围内退耕还林与还草后的团聚体有机碳含量与坡耕地相比总体表现出减小的趋势。研究结果表明,退耕改善了土壤结构,对各粒径团聚体有机碳含量分布的影响随退耕年限与方式不同效应各异,且GL15相较于其它退耕年限和方式下的样地有更好的土壤团聚体稳定性和更多的团聚体有机碳积累。     

不同温度下添加绿肥对旱作农田土壤有机碳矿化的影响

为揭示气候变暖背景下绿肥添加对旱作农田土壤有机碳矿化的影响,采用室内恒温培养法,研究了添加长武怀豆(S)、黑麦草(R)、长武怀豆与黑麦草混合(M)在5℃、15℃、25℃下的土壤有机碳矿化过程。结果表明:培养温度和绿肥种类及其二者交互作用对土壤有机碳矿化速率均具有显著影响。在15℃和25℃下有机碳矿化速率峰值均出现在培养开始后第2天,然后快速下降并分别在第17天和第22天后趋于稳定;而在5℃下有机碳矿化速率峰值则推迟至第8天出现,然后缓慢下降至第42天后趋于稳定。在为期79 d的培养期间,土壤有机碳平均矿化速率和累积矿化量均随着温度升高而增加。与不添加绿肥的对照(CK)相比, S、M和R处理土壤有机碳累积矿化量提高了10.5～11.6倍(P<0.05),绿肥处理间变化趋势为S>M>R,与其本身含碳量相一致。与CK相比,S、M和R处理土壤温度敏感性(Q₁₀)分别降低了11.0%、11.2%和11.8%。绿肥添加和增温同时还提高了土壤有机碳矿化动力学参数,其中S处理在不同温度下均较其他处理具有更高的土壤有机碳矿化速率常数。与CK相比,土壤碳素和氮素水平...     

不同耕作措施对(土娄)土土壤有机碳形态及活性的影响

为了探明不同耕作措施对土壤有机碳形态和活性的影响,以关中地区小麦、玉米轮作条件下,历时7 a不同耕作方式(深松、旋耕、免耕、传统耕作)的定位试验为研究对象,测定了不同土层土壤的总有机碳,高、中活性有机碳含量以及松结态、稳结态、紧接态有机碳含量,并计算了松结态有机碳与紧结态有机碳的比值(松/紧)。结果表明,与传统耕作比较,在小麦秸秆高留茬情况下,无论玉米秸秆是否还田,旋耕、深松和免耕处理均既能提高土壤有机碳含量,又能提高土壤的活性有机碳和松结态有机碳含量,并提高松结态有机碳与紧结态有机碳的比值,而深松和旋耕的效果比免耕明显,是关中地区比较理想的耕作模式。     

秸秆覆盖对宁南早作农田活性有机质及碳库管理指数的影响

在宁南半干旱区早作农田连续进行了4 a不同秸秆覆盖量的冬小麦栽培试验,对不同秸秆覆盖量下的土壤碳库活度(A)、碳库活度指数(AI)、碳库指数(CPI)和土壤碳库管理指数(CMPI)进行了分析.结果表明:与不覆盖(CK)相比,0.9-0.6万kg/hm2覆盖量下0～20 cm土层土壤总有机碳含量显著提高1.46～1.01...     

盐渍化弃耕地不同恢复年限土壤有机碳及其碳库管理指数变化

对干旱区盐渍化弃耕地不同恢复年限土壤有机碳及其碳库管理指数的变化进行分析,结果表明,弃耕地恢复初期土壤有机碳及活性有机碳（LOC）含量均低于弃耕地（CK）,恢复3年（R3）、恢复5（R5）年和恢复10（R10）年的 LOC 都显著高于弃耕地,分别高出20．28％、16．00％和16．45％,土壤有机碳及活性有机碳含量均随着土层加深而降低,土壤碳库管理指数 CMI 在恢复初期低于 CK ,随着恢复年限的增加,R3,R5,R10土壤 CMI 显著高于CK 54．72％、19．79％和17．73％,R3、R5和 R10分别是 R1的3．20、2．48 和 2．43倍,表明干旱区盐渍化弃耕地经垦殖恢复后显著改善了土壤碳库质量,增加了土壤碳汇功能。相关分析表明,土壤 LOC 和 CMI 与土壤 Olsen－P 呈显著正相关关系,与 TOC 相比更能反映不同恢复年限土壤碳库的变化。     

生态转型模式对吕梁山红枣经济林土壤团聚体及其有机碳分布的影响

为探究吕梁山区红枣经济林不同生态转型模式对土壤团聚体及其有机碳分布的影响,试验选取该地区5种主要的生态转换模式,分别为枣林撂荒(AF)、枣林补种黄芪-柴胡(MM)、补种苜蓿(AL)、补植油松(CP)、补植侧柏(PO),并以清耕枣林为对照(CK),测定并分析各样地0～20 cm土层中土壤团聚体稳定性、团聚体有机碳与土壤总有机碳含量及其相关性。结果表明：(1)与CK相比,除AF模式外,其他生态模式提高了>2.0 mm及>0.25 mm团聚体含量,增量分别为3.75%～9.31%和1.68%～10.36%;同时提高了团聚体的平均重量直径、几何平均直径,增量分别为0.05～0.19、0.03～0.10 mm, CP模式提高幅度最大;(2)所有生态模式显著提高了土壤有机碳含量,增量为0.24～4.72 g·kg^-1,提高幅度为9.25%～182.10%,同时提高了土壤各粒径团聚体有机碳含量;(3)土壤有机碳的贡献率主要来自于>0.25 mm团聚体,所有生态模式均提高了土壤>0.25 mm团聚体有机碳的贡献率,增量为4.20%～22.96%;(4)土壤...     

Biomass and carbon stocks in three types of Persian oak (Quercus brantii var. persica) of Zagros forests in a semi-arid area,Iran

Persian oak (Quercus brantii var. persica) is a dominant tree species of Zagros forests in a semi-arid area, western Iran. However, the capacity of biomass and carbon stocks of these forests is not well studied. We selected three types of oak, i.e., seed-originated oak, coppice oak and mixed (seed-originated and coppice) oak of Zagros forests in Dalab valley, Ilam Province, Iran to survey the capacity of biomass and carbon stocks in 2018. Thirty plots with an area of 1000 m² were systematically and randomly assigned to each type of oak. Quantitative characteristics of trees, such as diameter at breast height (DBH), height, crown diameter and the number of sprouts in each plot were measured. Then, aboveground biomass (AGB), belowground biomass (BGB), aboveground carbon stock (AGCS) and belowground carbon stock (BGCS) of each tree in plots were calculated using allometric equations. The litterfall biomass (LFB) and litterfall carbon stock (LFCS) were measured in a quadrat with 1 m×1 m in each plot. One-way analysis of variance and Duncan's test were performed to detect the differences in biomass and carbon stocks among three types of oak. Results showed that AGB, BGB and BGCS were significantly different among three types of oak. The highest values of AGB, AGCS, BGB and BGCS in seed-originated oak were 76,043.25, 14,725.55, 36,737.79 and 7362.77 kg/hm², respectively. Also, the highest values of LFB and LFCS in seed-originated oak were 3298.33 and 1520.48 kg/hm², respectively, which were significantly higher than those of the other two types of oak. The results imply the significant role of seed-originated oak for the regeneration of Zagros forests. Further conservation strategy of seed-originated oak is an important step in the sustainable management of Zagros forests in Iran.     

川西北高寒沙地红柳灌丛内外有机碳及腐殖质碳组分变化特征

为了解川西北高寒沙地红柳对土壤有机碳及腐殖质碳组分的影响,选取了沙地上修复24 a的红柳灌丛作为研究对象,通过野外调查并结合土壤样品采集和室内分析,研究了川西北沙地红柳灌丛根区(SR)、灌丛中部(SM)、灌丛边缘(SE)、灌丛外部(SO)的0~20,20~40 cm和40~60 cm土层土壤有机碳及腐殖质碳组分变化特征。结果表明:随着距灌丛植株水平距离的增加,土壤有机碳(SOC)、胡敏酸碳(HAC)、富里酸碳(FAC)和胡敏素碳(HMC)含量均呈现下降的特征;0~20 cm表层土壤,灌丛根区、灌丛中部和灌丛边缘土壤有机碳含量分别为灌丛外部的1.86倍、2.35倍和1.63倍,灌丛根区、灌丛中部和灌丛边缘土壤腐殖质碳含量分别为灌丛外部的1.96倍、0.68倍和1.22倍;在距灌丛植株水平距离相同条件下,随土层深度增加,土壤有机碳及腐殖质碳各组分含量呈降低趋势;在灌丛根区,20~40 cm和40~60 cm土层土壤有机碳相对于0~20 cm土层分别降低了32.31%和38.38%,20~40 cm和40~60 cm土层土壤腐殖质碳相对于0~20 cm土层分别降低了49.34%和53.40%。研究得出,红柳灌丛内外土壤有机碳及腐殖质碳组分存在空间异质性分布。     

青海湖环湖区表土有机碳氮储量估算

分析了沿青海湖湖岸采集的81个表土样品的总有机碳和氮含量得出：环湖区表土有机碳储量为27.81×10^6t,总氮储量为30.24×10^5t。占研究区面积最大的栗钙土,其表层土壤有机碳密度（8.19kg/m^2）显著高于同类研究,氮含量（3.63mg/g）亦高于青海省同类土壤的平均值,说明环湖区表土碳氮储量都是相当大的...     

地表覆盖对黄土高原土壤有机碳及其组分的影响

基于中国科学院长武黄土高原农业生态实验站2008年开始田间定位试验资料,分析研究秸秆覆盖与地膜覆盖对黄土高原土壤有机碳（SOC）及其组分的影响,试验包括5个处理：对照不覆盖（CK）、作物生育期9000 kg ·hm-2秸秆覆盖（M1）、作物生育期4500 kg·hm-2秸秆覆盖（M2）、夏闲秸秆覆盖（SF）、作物生育期地膜覆盖（PM）。2010（干旱年）、2012（丰水年）两次测定结果表明：0～30 cm土层平均,与CK相比,2012年土壤有机碳（SOC）含量M1处理提高了7．4％,潜在矿化碳（PCM）含量M1、M2、SF处理分别提高了37．8％、23．9％、7．2％,微生物量碳（MBC）含量M1和M2处理分别提高了59．9％和42．3％,碳库管理指数（CMI）M1、M2、SF 处理分别提高了53．1％、35．6％、13．9％;2010年M1处理CMI较CK提高了16．1％（P＜0．05）,其余处理土壤有机碳各指标与CK差异两年均不显著。不同覆盖方式对表层土壤有机碳及各项指标影响较大,随土层加深影响减弱,其中秸秆覆盖4年后碳库管理指数均有显著提高。两种活性有机碳的相对含量与其各自绝对含量的变化基本一致,且有机碳各指标间显著相关。综合来看,高量秸秆覆盖能够提高表层土壤有机碳及其组分含量,地膜覆盖对土壤有机碳及其组分积累影响不大。     

土地利用对陕北水土流失区土壤有机碳、水分的影响

通过实地调查和采样,结合室内分析,研究了当地四种土地利用方式(果园、林地、草地、坡耕地)下土壤有机碳分布特征.结果表明:流域内所有土样土壤有机碳(SOC)含量的均值为13.13g·kg-1.其中,坡耕地的土壤有机碳均倩为12.93g·kg-1,与坡耕地相比,果园土壤有机碳均值(12.97g·kg-1)略有升高;草地和林...