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Field trial on use of soybean crude extract for carbonate precipitation and wind erosion control of sandy soil 被引量:17
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作者 GAO Yu-feng MENG Hao +2 位作者 HE Jia QI Yong-shuai HANG Lei 《Journal of Central South University》 SCIE EI CAS CSCD 2020年第11期3320-3333,共14页
Wind erosion is a major cause of land desertification and sandstorm formation in arid and semi-arid areas.The objective of this study was to evaluate the potential of soybeans crude extract induced calcium carbonate p... Wind erosion is a major cause of land desertification and sandstorm formation in arid and semi-arid areas.The objective of this study was to evaluate the potential of soybeans crude extract induced calcium carbonate precipitation(SICP)on reducing wind erosion risk of sandy soil.Field tests were carried out in Ulan Buh Desert,Ningxia Hui Autonomous Region,China.Results showed that the SICP method could significantly enhance the surface strength and wind erosion resistance of the topsoil.The optimal cementation solution(urea-CaCl2)concentration and spraying volume,according to experiments conducted on sandy land,were 0.2 mol/L and 4 L/m^2,respectively.Under this condition,the CaCO3 content was approximately 0.45%,the surface strength of sandy soil could reach 306.2 kPa,and the depth of wind erosion was approximately zero,after 30 d completion of SICP treatment.Soil surface strength declined with the increase of time,and long-term sand fixation effects of SICP treatment varied depending on topography.Whereas wind erosion in the top area of the windward slope was remarkable,sandy soils on the bottom area of the windward slope still maintained a relatively high level of surface strength and a low degree of wind erosion 12 month after SICP treatment.Scanning electron microscopy(SEM)tests with energy dispersive X-ray(EDX)confirmed the precipitation of CaCO3 and its bridge effect.These findings suggested that the SICP method is a promising candidate to protect sandy soil from wind erosion in desert areas. 展开更多
关键词 soybeans crude extract induced calcium carbonate precipitation(SICP) biocementation sandy soil erosion controll field tests
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Pool Sizes and Turnover of Soil Organic Carbon of Farmland Soil in Karst Area of Guilin 被引量:3
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作者 YANG Hui CAO Jianhua +2 位作者 ZHANG Liankai HOU Yanlin MAO Lifeng 《Journal of Northeast Agricultural University(English Edition)》 CAS 2011年第1期39-45,共7页
The three-pool and first-order model separates the mineralizable organic carbon into active,slow,and passive carbon pools.This paper used the model and decomposition curves of the soil organic carbon to fit the active... The three-pool and first-order model separates the mineralizable organic carbon into active,slow,and passive carbon pools.This paper used the model and decomposition curves of the soil organic carbon to fit the active pool and its decomposition rate,slow pool and its decomposition rate.The results showed that the size of the active pool from different profiles accounted for 2.09%-3.08% of the total soil organic carbon and the mean residue time was 3.57-17.21 days.And the size of the slow pool accounted for 3.19%-43.55% and the mean residue time was 1.12-4.94 years.Acid hydrolysis(6M HCl) was used to fractionate the passive organic carbon,which accounted for 50.83%-94.44% of the total soil organic carbon. 展开更多
关键词 karst area FARMLAND soil organic carbon pool turnover time
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Biochar Serves as a Long-term Soil Carbon Pool 被引量:1
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作者 Lena Q.Ma 《地学前缘》 EI CAS CSCD 北大核心 2009年第S1期231-232,共2页
Biochar is a carbon-rich(】60%)organic material derived from incomplete combustion of fossil fuels and biomass.It consists of a continuum ranging from slightly charred material through char and charcoal to soot,and is... Biochar is a carbon-rich(】60%)organic material derived from incomplete combustion of fossil fuels and biomass.It consists of a continuum ranging from slightly charred material through char and charcoal to soot,and is ubiquitous in the atmosphere,marine sediment,soil and water.Moreover,】80%of biochar produced ends up in soils,where it resides for hundreds to thousands of years.Because of its resistance to biological and chemical breakdown, biochar can serve as a pool of C with long residence time in the soil.As a result,there has been increasing attention given to the potential of biochar to sequestrate carbon and counteract 展开更多
关键词 BIOCHAR soil carbon POOL carbon-based GREENHOUSE GASES
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Adsorption removal of endosulfan through Saccharum officinarum derived activated carbon from selected soils 被引量:2
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作者 Khuram Shahzad AHMAD 《Journal of Central South University》 SCIE EI CAS CSCD 2019年第1期146-157,共12页
Pesticide contamination causes precarious implications on human health and environment.Thus the investigation of its sorption phenomenon is highly imperative.Endosulfan insecticide was examined for its adsorption beha... Pesticide contamination causes precarious implications on human health and environment.Thus the investigation of its sorption phenomenon is highly imperative.Endosulfan insecticide was examined for its adsorption behavior on ten assorted soils through batch equilibrium method.Adsorption coefficient values(Kd)ranged from 1.4μg/mL to 18μg/mL.The highest Kd value was obtained for Peshawar soil owing to the presence of highest amount of organic matter(1.4%).Negative values of Gibbs free energy displayed a low interaction between soil and pesticide,exhibiting that the reaction was physiosorption and exothermic in nature.Statistical analysis showed a negative correlation of soil pH and Kd(R^2=–0.77 and p=0.03)and a positive correlation with organic matter(R^2=0.96).Activated carbon prepared from Saccharum officinarum bagasse removed significant amount pesticide.The maximum removal observed was 93%and 97%in 5×10^–6 and 7.5×10^–6,respectively.Activated carbon prepared from biomass for removal purposes was proved to be highly efficient and cost effective. 展开更多
关键词 soil ENDOSULFAN ADSORPTION activated carbon sugarcane husk
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Effects of Carbon and Nitrogen Additions on Soil Microbial Biomass Carbon and Enzyme Activities Under Rice Straw Returning 被引量:2
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作者 Dai Jian-jun Liu Li-zhi +4 位作者 Wang Xiao-chun Fang Qiu-na Cheng Ye-ru Wang Dan-ni Peng Xian-long 《Journal of Northeast Agricultural University(English Edition)》 CAS 2021年第3期21-30,共10页
The effects of different amounts of carbon and nitrogen sources on the soil microbial biomass carbon,dissolved organic carbon and related enzyme activities were studied by the simulation experiment of rice straw retur... The effects of different amounts of carbon and nitrogen sources on the soil microbial biomass carbon,dissolved organic carbon and related enzyme activities were studied by the simulation experiment of rice straw returning to the field,and the mechanism of the decomposition of rice straw returning to the field was discussed.Completely randomized experiment of the two factors of the three levels was designed,and a total of nine treatments of indoor soil incubation tests were conducted.Full amount of rice straw was applied to the soil in this simulation experiment and different amounts of brown sugar and urea were added in the three levels of 0(no carbon source and nitrogen source),1(low levels of carbon and nitrogen sources)and 2(high levels of carbon and nitrogen sources),respectively.The results showed that the addition of different amounts of carbon and nitrogen sources to the rice straw could increase the soil carbon content.Compared with T0N0,the microbial biomass carbon of T2N2 was increased significantly by 170.48%;the dissolved organic carbon content of T1N2 was significantly increased by 58.14%and the free humic acid carbon contents of T0N2,T1N1 and T2N0 were significantly increased by 56.16%and 45.55%and 47.80%,respectively;however,there were no significant differences among those of treatments at later incubation periods.The addition of different carbon and nitrogen sources could promote the soil enzyme activities.During the incubation period,all of the soil enzyme activities of adding sugar and urea were higher than those of T0N0 treatment.Therefore,the addition of different amounts of carbon and nitrogen sources to rice straw returning could improve soil microbial biomass carbon content,dissolved organic carbon and soil enzyme activities. 展开更多
关键词 rice straw returning carbon and nitrogen sources microbial biomass carbon dissolved organic carbon soil enzyme activity
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Characteristics of soil organic carbon andtotal nitrogen storages for differentland-use types in Central Yunnan Plateau 被引量:1
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作者 SHEN Fangyuan TUO Yunfei +4 位作者 WANG Qian WANG Fei ZHENG Yang DU Wenjuan XIANG Ping 《排灌机械工程学报》 CSCD 北大核心 2022年第5期519-528,共10页
Two-factor analysis of variance and redundancy analysis were used to analyze the characte-ristics of soil organic carbon total nitrogen storage in garden land,forestland,grassland,farmland,and bare land in the Dachunh... Two-factor analysis of variance and redundancy analysis were used to analyze the characte-ristics of soil organic carbon total nitrogen storage in garden land,forestland,grassland,farmland,and bare land in the Dachunhe watershed of Jinning District,Kunming City,Yunnan Province,China.The effects of the soil organic carbon,total nitrogen stratification ratio,soil physical and chemical factors on the storage characteristics of organic carbon and total nitrogen of different land-use types were analyzed.The results show that the rates of carbon and nitrogen stratification in soil from 0-20 cm and 40-60 cm of the same land-use types differed are statistically significant(P<0.05).The organic carbon and total nitrogen stratification ratio SR1 of garden land soil are 38.5%and 25.3%,respectively,which are higher than SR^(2).The soil organic carbon and total nitrogen stratification ratio SR^(2) of different land-use types are greater than SR1.There are statistically significant differences in the SR^(2) soil organic carbon and total nitrogen stratification ratios(P<0.05).Soil organic carbon and total nitrogen storage of diffe-rent land-use types gradually decrease with increasing soil depth,with the maximum soil organic carbon and total nitrogen storage in the 0-20 cm soil layer.Soil organic carbon and total nitrogen sto-rage at the same soil depth are significantly different(P<0.05).Soil organic carbon and total nitrogen storage in the garden land are greater than those in the other land-use types.Soil organic carbon and total nitrogen storage in 0-20 cm garden land are 4.96 and 3.19 times than those in bare land,respectively;soil organic carbon and total nitrogen storage are explained by 93.66%and 1.53%in redundancy analysis RDA1 and RDA2,respectively.All physicochemical factors except Available Phosphorus and pH are statistically significance with carbon and nitrogen storage(P<0.05).Soil cationic exchange capacity,Available Phosphorus,C/N ratio,and Moisture Content are positively correlated with organic carbon and total nitrogen storage.In contrast,soil Bulk Density is negatively correlated with organic carbon storage and total nitrogen storage.Available Phosphorus,C/N ratio,and Moisture Content are the main factors promoting soil organic carbon and total nitrogen accumulation. 展开更多
关键词 soil organic carbon storage soil total nitrogen storage stratification ratio land-use types Central Yunnan Plateau
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Soil Carbon Sequestration,Water Use Efficiency(WUE) and Biological Nitrogen Fixation(BNF) Under Conservation Agriculture in Rain-fed Dry Area of North-west Pakistan
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作者 Samreen Shehzadi Wisal Mohammad S.Mahmood Shah 《地学前缘》 EI CAS CSCD 北大核心 2009年第S1期233-233,共1页
Land degradation,unbalanced nutrition,change in climate and its extreme variability are the factors affecting the sustainability of agriculture and food security.In North-west Pakistan,more than 50%of the cultivated a... Land degradation,unbalanced nutrition,change in climate and its extreme variability are the factors affecting the sustainability of agriculture and food security.In North-west Pakistan,more than 50%of the cultivated area is rain-fed and the crop productivity is low.Conservation agriculture reduces greenhouse gas emissions by enhancing soil carbon sequestration and then improved soil fertility,WUE and crop productivity.A field experiment 展开更多
关键词 soil carbon sequestration BNF water use efficiency crop residue TILLAGE soil microbial biomass C and N
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Distribution of soil water-stable aggrega-tes and organic carbon content affected by tillage systems:a meta-analysis
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作者 LU Xingli LI Shanshan +4 位作者 LIU Jihu DUAN Yaxin YUE Heng KANG Jianhong WU Hongliang 《排灌机械工程学报》 CSCD 北大核心 2021年第10期1051-1055,共5页
A better understanding of soil carbon(C)distribution within aggregate fractions is essential to evaluating the potential of no-till for sustaining productivity and protecting the environment.A meta-analysis on 744 com... A better understanding of soil carbon(C)distribution within aggregate fractions is essential to evaluating the potential of no-till for sustaining productivity and protecting the environment.A meta-analysis on 744 comparisons from 34 studies was conducted to determine the effects of three different tillage treatments(conventional mouldbould ploughing tillage(CT),reduced tillage(RT)and no tillage(NT))on water-stable aggregate size distribution,soil C concentration in aggregate fractions.The meta-analysis indicates that compared with CT treatment,NT/RT significantly(P<0.05)increases macro-aggregate above 20 cm by 20.9%-82.2%(>2.00 mm)and 5.9%-19.1%(0.25-2.00 mm),whereas NT/RT significantly reduces micro-aggregate and silt clay fractions above 20 cm.NT/RT significantly(P<0.05)increases the SOC in macro-aggregate(>0.25 mm)and micro-aggregate(<0.25 mm)size classes above 20 cm soil depth compared with CT.The results suggest that soil sampling depth should be considered to evaluate the influence of tillage systems on the distribution of soil aggregate,and the content of aggregate-associated C content. 展开更多
关键词 soil aggregation soil organic carbon reduced tillage soil depth
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Key Physical Factors Affecting Spatial-temporal Variation of Labile Organic Carbon Fractions by Biochar Driven in Mollisols Region of Northeast China
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作者 Zhao Wei Liang Fangyuan +4 位作者 Liang Ying Zhao Hongrui Hao Shuai Wang Hongyan Wang Daqing 《Journal of Northeast Agricultural University(English Edition)》 CAS 2024年第1期28-41,共14页
Biochar is widely used to improve soil physical properties and carbon sequestration. However, few studies focuse on the impact of maize stalk biochar on labile organic carbon(LOC) pool and the relationship between phy... Biochar is widely used to improve soil physical properties and carbon sequestration. However, few studies focuse on the impact of maize stalk biochar on labile organic carbon(LOC) pool and the relationship between physical properties and LOC fractions. A field positioning experiment was performed in Mollisols region of Northeast China to evaluate the influence of maize stalk biochar on the spatial distribution and temporal changes of physical properties and LOC fractions. Maize stalk biochar treatments included C1(1.5 kg·hm^(-2)), C2(3 kg·hm^(-2)), C3(15 kg·hm^(-2)), C4(30 kg·hm^(-2)), and CK(0). The results showed that maize stalk biochar increased soil water contents(SWC) and soil porosity(SP), but reduced bulk density(BD). Maize stalk biochar reduced dissolved organic carbon(DOC) contents in the 0-20 cm soil layer, ranging from 0.25 g·kg^(-1) to 0.31 g·kg^(-1) in harvest period, while increased in the 20-40 cm soil layer. In addition, the application of biochar had a significant impact on the spatial distribution and temporal change of SWC, BD, SP, DOC, hot-water extractable carbon(HWC), acid hydrolyzed organic carbon(AHC Ⅰ, Ⅱ), and readily oxidized organic carbon(ROC). High amounts of maize stalk biochar up-regulated the contents of soil organic carbon SOC, HWC, AHC Ⅰ, AHC Ⅱ, and ROC. In addition, SWC and SP were the key physical factors to affect LOC fractions. In conclusions, maize stalk biochar could improve physical properties, and then influence LOC fractions, and maize stalk biochar could be used as an organic amendment for restoring degraded soils governed by their rates of addition. 展开更多
关键词 maize stalk biochar labile organic carbon fraction Mollisols region soil physical property dissolved organic carbon
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森林土壤储碳与增汇的不确定性分析 被引量:1
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作者 王晖 刘世荣 +2 位作者 周正虎 陈亮 王健 《生态学报》 北大核心 2025年第8期3626-3644,共19页
森林具有类型多样、结构复杂以及随环境变化等特征,1 m深森林土壤储存的碳约占全球森林生态系统总碳储量的45%,约占全球土壤碳库的52%。目前对森林土壤固碳潜力和关键过程机制的认识还十分有限。因此,森林土壤储碳与增汇的估算仍存在很... 森林具有类型多样、结构复杂以及随环境变化等特征,1 m深森林土壤储存的碳约占全球森林生态系统总碳储量的45%,约占全球土壤碳库的52%。目前对森林土壤固碳潜力和关键过程机制的认识还十分有限。因此,森林土壤储碳与增汇的估算仍存在很大不确定性。研究梳理了森林土壤有机碳(SOC)储量、密度、含量、增量、固定和碳汇等术语定义;综述了SOC稳定性的机制,包括化学结构稳定性、团聚体物理保护、金属氧化物和粘土矿物吸附,生物与环境主导有机碳稳定固持,以及最新研究相继提出的森林SOC组分多样性及功能复杂性维持碳稳定的学术观点。研究还分析了森林SOC储量和增量不同测定方法的主要原理、优点和不足。根据已有文献数据分析,全球森林1 m深SOC储量变化范围为383—787 Pg C(Pg=10^(15)g),年变化范围为每年降低349 Tg C(Tg=10^(12)g)到每年增加498 Tg C。中国森林1 m深SOC储量评估范围为16.0—34.2 Pg C,年变化范围为每年降低64.5 Tg C到增加217.3 Tg C。说明目前对森林SOC储量和增量的估算还存在很大不确定性。最新研究表明全球森林碳容量和固碳潜力巨大,但不同研究对SOC是否存在上限仍具不同观点,气候变化对森林SOC储量及其持续固碳潜力的影响也存在较大的不确定性。未来建议通过学科交叉深入探索森林群落结构与土壤固碳过程之间的联系,从碳组分多样性和功能复杂性的新视角理解森林SOC的形成与稳定机制;将SOC监测纳入国家森林资源清查体系、建立国家尺度的SOC长期监测网络、设立我国森林SOC增汇大科学计划;提出保持SOC稳定固持的天然林保护修复及经营提升途径;建立培育高固碳树种,优化林分结构,合理采伐以及轮伐期延长等人工林土壤固碳增汇经营技术体系。 展开更多
关键词 森林土壤 储碳 增汇 固碳潜力 不确定性
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绿肥部分替代化肥氮对土壤物理性状的影响 被引量:1
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作者 秦文利 张静 +10 位作者 肖广敏 崔素倩 叶建勋 智健飞 张立锋 谢楠 冯伟 刘振宇 潘璇 代云霞 刘忠宽 《草业学报》 北大核心 2025年第6期27-45,共19页
2020-2022年度以毛叶苕子和玉米为材料,采用二因素裂区田间试验设计,主处理为冬闲田(FF)、冬闲田种植毛叶苕子并全量还田(HV)2种模式,副处理为玉米0(0N)、135.0(50%N)和270.0 kg·hm^(-2)(100%N)3个施氮水平,研究了毛叶苕子还田和... 2020-2022年度以毛叶苕子和玉米为材料,采用二因素裂区田间试验设计,主处理为冬闲田(FF)、冬闲田种植毛叶苕子并全量还田(HV)2种模式,副处理为玉米0(0N)、135.0(50%N)和270.0 kg·hm^(-2)(100%N)3个施氮水平,研究了毛叶苕子还田和施氮水平对玉米0~10 cm、10~20 cm土层土壤团聚体组成与分布、团聚体平均重量直径(MWD)、几何平均直径(GMD)、破坏率(PAD)、可蚀性因子(K)、容重(BD)、总孔隙度(TP)、毛管孔隙度(CP)、非毛管孔隙度(NCP)、最大持水量(MWHC)、毛管持水量(CWHC)、非毛管持水量(NCWHC)、土壤有机碳(SOC)含量、团聚体有机碳(AOC)含量及玉米产量的影响,以期从土壤物理性状变化为绿肥部分替代化肥氮实现作物稳产增产提供科学依据。结果表明,与FF模式相比,HV模式0~10 cm、10~20 cm土层>0.25 mm水稳定性团聚体总含量(R0.25)、MWD、GMD、TP、CP、NCP、MWHC、CWHC、NCWHC、SOC含量分别显著增加8.95%、40.84%、30.57%、5.89%、1.47%、4.42%、15.01%、6.41%、27.08%、7.29%和13.13%、62.87%、51.68%、5.02%、0.76%、4.25%、13.11%、3.32%、27.86%、7.10%;PAD、K和BD分别显著降低8.83%、20.79%、5.99%和12.14%、30.73%、7.31%。HV模式下各土层各粒径AOC含量及玉米产量均显著提高。施氮水平对各土层各粒径AOC含量、R0.25及其他物理性状指标、玉米产量影响显著或极显著。HV模式50%N处理0~10 cm、10~20 cm土层的SOC含量、>5 mm AOC含量及0~10 cm土层的0.50~1.00 mm AOC含量、10~20 cm土层的BD、TP、CP、NCP、MWD、CWHC、NCWHC及玉米产量较FF模式100%N处理变化均不显著,0~10 cm、10~20 cm土层的2.00~5.00 mm、1.00~2.00 mm、0.25~0.50 mm、<0.25 mm AOC含量及10~20 cm土层0.50~1.00 mm的AOC含量,0~10 cm、10~20 cm土层的R0.25、MWD、GMD,0~10 cm土层的TP、NCP、MWHC、NCWHC均显著提高,0~10 cm、10~20 cm土层的PAD、K及0~10 cm土层的BD均显著下降。各粒径AOC含量与SOC含量之间、各粒级团聚体含量与其AOC含量之间、土壤物理性状指标与各粒级团聚体含量之间、玉米产量与土壤物理性状指标之间均呈显著或极显著相关。因此,绿肥还田后土壤有机碳含量的提高是促进团粒结构形成,增强土壤抗侵蚀、持水能力的重要基础。绿肥对土壤氮、有机碳的输入是其部分替代氮肥、改善土壤物理性状、实现减氮增产的重要前提。 展开更多
关键词 毛叶苕子 施氮水平 土壤有机碳含量 土壤物理性状 玉米产量
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滨海盐碱地绿肥粉垄耕作耦合对土壤有机碳积累及组分的影响 被引量:1
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作者 洪立洲 邢锦城 +7 位作者 乔干群 刘冲 张振华 郁凯 董静 朱小梅 陈环宇 王同 《江苏农业学报》 北大核心 2025年第1期61-67,共7页
为了明确绿肥粉垄耕作耦合对改良盐碱地的作用,本研究采用田间试验探索了滨海盐碱地绿肥粉垄耕作耦合对土壤有机碳积累及组分的影响。小区试验设置了6个处理:裸地+免耕(CK),裸地+常规耕作15 cm深(T1),裸地+粉垄耕作30 cm深(T2),种植苕... 为了明确绿肥粉垄耕作耦合对改良盐碱地的作用,本研究采用田间试验探索了滨海盐碱地绿肥粉垄耕作耦合对土壤有机碳积累及组分的影响。小区试验设置了6个处理:裸地+免耕(CK),裸地+常规耕作15 cm深(T1),裸地+粉垄耕作30 cm深(T2),种植苕子并离田+常规耕作15 cm深(T3),种植苕子并还田+常规耕作翻压15 cm深(T4),种植苕子并还田+粉垄耕作30 cm深(T5)。通过采集种植一季玉米后0~20 cm土壤样品,测定了土壤样品基本理化性状,分析了水稳性团聚体、团聚体有机碳的变化,土壤有机碳积累及组分的变化特征。结果表明,与CK相比,种植绿肥并翻压可显著促进盐碱地土壤有机碳的积累,提高土壤有机碳含量,改善土壤有机碳组成。与CK相比,T5处理土壤容重明显降低,土壤碱解氮含量、有机质含量、有机碳含量及有机碳储量均显著提高,其中,土壤有机碳含量提高幅度达到32.9%;土壤可溶性有机碳含量、易氧化有机碳含量、微生物生物量碳含量显著提高;>2.000 mm、0.251~2.000 mm粒级土壤团聚体重量百分数提高,而0.050~0.250 mm、<0.050 mm粒级土壤团聚体重量百分数降低。T5处理提高了水稳性团聚体中有机碳含量及团聚体中有机碳贡献率。由此可见绿肥粉垄耕作耦合可以显著提高滨海盐碱地土壤有机碳及活性组分含量,有效提升土壤水稳性大团聚体比例以及土壤团聚体中有机碳含量及其有机碳贡献率。因此,该耕作方式在滨海盐碱地上推广应用,可促进土壤有机碳的积累,从而达到改善滨海盐碱地土壤碳封存,提高滨海盐碱地土壤耕地质量的目的。 展开更多
关键词 滨海盐碱地 绿肥粉垄耕作耦合 有机碳 土壤团聚体
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甘肃尕海湿地不同植被退化阶段土壤颗粒有机碳含量及动态 被引量:1
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作者 马维伟 刘强 +1 位作者 李广 常文华 《土壤学报》 北大核心 2025年第1期189-200,共12页
研究高寒湿地植被退化过程中土壤颗粒有机碳(POC)的变化特征及其影响因素,可为深入理解高寒湿地土壤碳库动态对气候变化和人类活动的响应提供基础数据。以甘肃尕海湿地区内不同植被退化程度的沼泽草甸(未退化ND、轻度退化SD、中度退化M... 研究高寒湿地植被退化过程中土壤颗粒有机碳(POC)的变化特征及其影响因素,可为深入理解高寒湿地土壤碳库动态对气候变化和人类活动的响应提供基础数据。以甘肃尕海湿地区内不同植被退化程度的沼泽草甸(未退化ND、轻度退化SD、中度退化MD和重度退化HD)湿地土壤为研究对象,研究了植被退化过程中湿地土壤POC在2016年和2017年生长季的变化特征及其与环境之间的关系。结果表明:(1)植被退化显著降低了湿地表层(0~10和10~20 cm)土壤POC含量,而对其他土层(20~40、40~60、60~80和80~100 cm)土壤POC含量影响不显著。(2)随生长季的推移,表层土壤POC含量呈现先降后升的趋势,但其他土层土壤POC含量无明显变化,2016年土壤POC含量和变幅均高于2017年。(3)采样时间、植被退化和土壤深度均对POC影响显著,同时对土壤POC有显著交互作用。(4)全氮和地下生物量是影响土壤有机碳组分变化的主导因素。植被退化可能导致青藏高原湿地表层土壤碳库中积累的大量POC损失,使青藏高原湿地成为一个潜在碳源。 展开更多
关键词 植被退化 土壤颗粒有机碳 时空分布 尕海湿地
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长期增施有机肥对土壤物理特征、微生物生物量碳氮及土壤酶活性的影响
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作者 杨永辉 张运红 +5 位作者 高翠民 刘昊 潘晓莹 何方 韩伟锋 武继承 《干旱地区农业研究》 北大核心 2025年第3期107-115,共9页
增施有机肥对改善土壤结构、提高土壤保水保肥能力,提升微生物活性和土壤质量均具有重要作用,但长期增施有机肥对土壤物理特性、水分参数、微生物特性及其相互关系尚不清楚,需要系统研究以确定长期施用有机肥对于土壤理化特性及其生物... 增施有机肥对改善土壤结构、提高土壤保水保肥能力,提升微生物活性和土壤质量均具有重要作用,但长期增施有机肥对土壤物理特性、水分参数、微生物特性及其相互关系尚不清楚,需要系统研究以确定长期施用有机肥对于土壤理化特性及其生物特性的综合作用效果。本研究在河南省节水农业禹州试验基地开展长期定位试验(2006年小麦播种时开始),采用CT扫描技术定量分析长期施用有机肥(腐熟鸡粪750 kg·hm^(-2))对0~40 cm土层土壤孔隙的影响,同时测定分析0~10 cm土层的土壤团粒结构、土壤水分参数及微生物生物量碳氮和土壤酶活性等指标。结果表明:随着土壤团聚体粒级的减小,不同施肥措施的土壤团聚体含量表现为逐渐增加的趋势。与单施化肥相比,增施有机肥的>0.5 mm粒级的团聚体含量提高了70.1%,0.25~0.5 mm和<0.25 mm粒级的团聚体含量分别减少了34.2%和26.5%;增施有机肥提高了水稳性大团聚体含量和团聚体平均重量直径,提高了土壤结构稳定性。随土层的加深,土壤孔隙数目呈现逐渐增加的趋势,土壤孔隙度则表现为逐渐降低的趋势,土壤孔隙成圆率则表现为逐渐增加再降低的趋势。长期增施有机肥提高了0~100 mm、200~250 mm和250~300 mm土层的孔隙数目,0~100 mm、150~200 mm和250~400 mm土层的土壤孔隙度以及0~150 mm和155~200 mm土层的孔隙成圆率;长期增施有机肥可提高土壤饱和导水率、土壤持水能力、供水能力、田间持水量及有效水含量,且提高了小麦不同生育时期的土壤微生物生物量碳和氮、土壤蔗糖酶、纤维素酶、脲酶及蛋白酶活性。综上所述,长期增施有机肥改善了土壤理化性质、提高了土壤结构稳定性和土壤水分参数,同时提高了微生物活性和土壤酶活性。 展开更多
关键词 有机肥 土壤结构 土壤有机碳 土壤水分参数 土壤微生物生物量碳氮 土壤酶活性
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南小河沟流域水土保持碳汇能力评估研究 被引量:1
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作者 张西宁 曹丹 +3 位作者 李超 刘恭辅 靳琪 袁鹏超 《人民黄河》 北大核心 2025年第3期117-122,共6页
为探索黄土高原地区小流域综合治理碳汇能力评估方法,以黄土高塬沟壑区南小河沟流域为研究对象,把1952年在该流域内设立的水土保持综合治理试验场作为核算情景、未治理对比观测小流域董庄沟作为基线情景,通过遥感影像解译、无人机航测... 为探索黄土高原地区小流域综合治理碳汇能力评估方法,以黄土高塬沟壑区南小河沟流域为研究对象,把1952年在该流域内设立的水土保持综合治理试验场作为核算情景、未治理对比观测小流域董庄沟作为基线情景,通过遥感影像解译、无人机航测、野外调查等取得研究区土地利用情况,把人工林地划分为10个碳层进行样区设置、植被和土壤样品采集及理化指标测定,评估了人工林地增绿增汇、植物措施和淤地坝保土固碳、流域综合治理减蚀减排3种主要途径的碳汇能力。结果表明:人工林地增绿增汇能力为6.40 t/(hm^(2)·a),其中植被碳库、土壤碳库碳汇能力分别为5.85、0.55 t/(hm^(2)·a);植物措施保土固碳能力为0.92 t/(hm^(2)·a),淤地坝(坝地)保土固碳能力为30.84 t/(hm^(2)·a);流域综合治理减蚀减排能力为0.14 t/(hm^(2)·a)。淤地坝保土固碳能力最大但坝地面积相对较小、人工林地增绿增汇能力与淤地坝相比相对较小但面积较大、减蚀减排是通过优化土地管理措施减缓大气二氧化碳浓度上升的重要环节,三者相辅相成、不可偏废。建议:因地制宜大力兴建淤地坝,加强对水土保持林的管护和更新,各项治理措施协同配合,更好地发挥水土保持综合治理的碳汇作用,提高区域水土保持碳汇能力。 展开更多
关键词 水土保持 碳汇能力 增绿增汇 保土固碳 减蚀减排 评估 南小河沟流域
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热带砖红壤果园长期生草对土壤团聚体及有机碳分布的影响
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作者 赵秋芳 魏长宾 +5 位作者 马海洋 王成艳 马智玲 严程明 汤昕明 冼皑敏 《西南农业学报》 北大核心 2025年第1期145-151,共7页
【目的】研究热带砖红壤典型果园生草对土壤团聚体和有机碳固存的影响,为砖红壤果园土壤物理结构改良和有机碳提升提供理论支撑。【方法】以热带砖红壤番石榴果园为研究对象,设置清耕(CK)、自然生草(NG)、热研2号柱花草(Re)、Ubon柱花草... 【目的】研究热带砖红壤典型果园生草对土壤团聚体和有机碳固存的影响,为砖红壤果园土壤物理结构改良和有机碳提升提供理论支撑。【方法】以热带砖红壤番石榴果园为研究对象,设置清耕(CK)、自然生草(NG)、热研2号柱花草(Re)、Ubon柱花草(Ub)4个处理,对果园长期生草下土壤团聚体组成、团聚体稳定性及有机碳分布进行分析。【结果】5年长期果园生草试验的研究结果表明,果园生草处理显著增加0~20 cm土层>2 mm水稳性团聚体含量,降低了0.25~2.00和0.053~0.250 mm水稳性团聚体含量,同时显著增加了R_(0.25)、MWD和GWD,提高了0~20 cm土层团聚体稳定性,但对20~40 cm土层团聚体分布和稳定性影响不显著。果园生草处理显著增加了土壤有机碳含量,Re、Ub和NG处理0~20 cm土层有机碳含量较CK分别提高55.0%、37.3%和24.8%,20~40 cm土层有机碳含量较CK分别提高28.1%、42.7%和25.0%。柱花草(Re和Ub)处理显著提高0~20和20~40 cm土层中>2 mm和0.25~2.00 mm粒级有机碳含量及其对土壤有机碳的贡献率。【结论】研究表明热带果园长期生草特别是种植柱花草可显著提高土壤水稳性团聚体的稳定性,同时增加土壤有机碳含量,显著提高土壤水稳性大团聚体中有机碳分布,提高其对土壤有机碳的贡献率。 展开更多
关键词 砖红壤 果园生草 土壤团聚体 团聚体有机碳
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基于MICP技术的固化黏土抗侵蚀性能研究 被引量:1
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作者 张伟丽 李明依 +2 位作者 李俊 钱程 陈宗武 《安全与环境工程》 北大核心 2025年第1期201-210,232,共11页
近年来,微生物诱导碳酸钙沉积(MICP)技术被应用于表层土体的加固处理,以提升土体的抗侵蚀能力。采用新型的单相法和传统的两相法对黏性土表层进行MICP处理,分析了环境pH值和胶结液浓度对MICP反应过程的影响,并对经过不同处理次数的土样... 近年来,微生物诱导碳酸钙沉积(MICP)技术被应用于表层土体的加固处理,以提升土体的抗侵蚀能力。采用新型的单相法和传统的两相法对黏性土表层进行MICP处理,分析了环境pH值和胶结液浓度对MICP反应过程的影响,并对经过不同处理次数的土样进行冲刷试验,观察并记录冲刷试验过程中土样的质量变化,以此评价2种加固方法的效果。结果表明:采用MICP技术加固后,土壤颗粒之间形成了有效的胶结;使用单相法加固的土样中碳酸盐生成量少于两相法,但土体整体的水稳性高于两相法;经过单相法和两相法加固处理5次后,试样被冲刷40 s后的侵蚀量分别为0.43 g和0.11 g,而相同条件下未加固试样的侵蚀量为54.63 g,加固后的土样经过24 h的冲刷试验后表面几乎没有被破坏,显示采用MICP技术加固后土样的抗侵蚀能力远大于未处理土样。 展开更多
关键词 微生物诱导碳酸钙沉积(MICP)技术 黏土加固处理 冲刷试验 土壤抗侵蚀性能
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有机物料添加对黑垆土和黄绵土有机碳组分的影响
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作者 王丹丹 赵欢欢 +2 位作者 许晨阳 李江文 胡斐南 《水土保持通报》 北大核心 2025年第4期267-276,共10页
[目的]研究12种不同外源有机物料,包括烟杆生物炭、果木枝条生物炭、小麦秸秆、油菜秸秆、鸡粪、牛粪、葡萄糖、纤维素、LB培养基、聚丙烯酰胺(PAM)、腐植酸肥、壳聚糖,对典型黄土(黑垆土与黄绵土)理化特性及土壤有机碳组分的影响,为农... [目的]研究12种不同外源有机物料,包括烟杆生物炭、果木枝条生物炭、小麦秸秆、油菜秸秆、鸡粪、牛粪、葡萄糖、纤维素、LB培养基、聚丙烯酰胺(PAM)、腐植酸肥、壳聚糖,对典型黄土(黑垆土与黄绵土)理化特性及土壤有机碳组分的影响,为农田土壤质量提升过程中有机改良剂的选择与应用提供理论依据。[方法]将有机物料与风干土壤以3%的质量比混合,并进行100 d的室内培养试验,同时设置不添加有机物料为对照组(CK)。利用密度浮选结合湿筛的方法分离并计算土壤游离态颗粒有机碳(FPOC)、闭蓄态颗粒有机碳(OPOC)、颗粒态有机碳(POC)和矿质结合态有机碳(MOC)4个有机碳组分,通过冗余分析(RDA)对土壤理化性质与有机碳组分之间的关系进行解析。[结果]①与CK相比,有机物料添加能够有效降低两种典型黄土的碳酸钙含量,提高土壤电导率、TOC以及全氮(纤维素添加除外)含量。②与CK相比,土壤中FPOC,OPOC,POC和MOC含量均有所提高,其中以果木枝条生物炭、烟杆生物炭、小麦秸秆添加处理下的FPOC增量最大,黑垆土中相应各指标分别提高了2158.5%,1545.3%,907.5%,黄绵土中各指标含量分别提高了2971.8%,1717.9%,1730.8%。③FPOC,OPOC,POC和MOC含量与TOC呈极显著的正相关关系(p<0.01)。C/N及全氮含量是影响土壤各组分有机碳含量的主要原因,其解释率在黑垆土和黄绵土中分别达到了76.1%和76.3%。[结论]有机物料添加使TOC含量升高,有效地改善了土壤理化性质,使土壤FPOC,OPOC,POC和MOC含量与CK相比均有所提高。C/N及全氮含量是影响土壤各组分有机碳含量的主控因素。 展开更多
关键词 秸秆 生物炭 颗粒态有机碳 有机碳组分 矿质结合态有机碳 黑垆土 黄绵土
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不同灌溉方式对设施土壤团聚体稳定性及有机碳含量的影响
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作者 邹洪涛 贺荣涛 +5 位作者 张一峰 任立军 范庆锋 虞娜 张玉玲 张玉龙 《沈阳农业大学学报》 北大核心 2025年第4期1-12,共12页
[目的]灌溉是设施作物获取水分的主要途径,不同灌溉方式影响土壤团聚体形成和稳定。除了受环境因子的影响,土壤团聚体的形成与胶结物质的种类和形态也密切相关。探究不同灌溉方式对设施土壤团聚体稳定性及有机碳的影响,为设施农业水分... [目的]灌溉是设施作物获取水分的主要途径,不同灌溉方式影响土壤团聚体形成和稳定。除了受环境因子的影响,土壤团聚体的形成与胶结物质的种类和形态也密切相关。探究不同灌溉方式对设施土壤团聚体稳定性及有机碳的影响,为设施农业水分调控、改善设施土壤结构提供理论依据。[方法]以连续12年采用不同灌溉方式(滴灌、渗灌和沟灌)进行番茄(华粉5号)栽培的设施土壤为研究对象,探究0~40 cm土壤团聚体稳定性及有机碳的含量与分布特征。[结果]通过湿筛法对团聚体组成及稳定性的分析发现,滴灌处理显著增加20~40 cm土层大团聚体含量,提高平均重量直径和几何平均直径,并降低平均重量比表面积和分形维数。滴灌处理显著增加20~40 cm土层大团聚体有机碳含量,大团聚体颗粒有机碳、微团聚体矿质结合态有机碳和易氧化有机碳含量也有所提高。冗余分析对团聚体相关有机碳的解释率为82.09%,其中大团聚体有机碳和微团聚体矿质结合态有机碳是对团聚体稳定性指标起主要贡献作用的有机碳。[结论]长期设施耕作条件下,滴灌更有利于提高土壤团聚体稳定性及有机碳含量。 展开更多
关键词 设施土壤 灌溉方式 团聚体 有机碳
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不同放牧强度对荒漠草原土壤活性有机碳的影响
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作者 张磊 张玉娟 +5 位作者 孙世贤 徐学宝 邢越 刘晓丽 高翠萍 王成杰 《草地学报》 北大核心 2025年第8期2541-2547,共7页
研究不同放牧强度对荒漠草原土壤活性有机碳的影响,了解放牧对土壤有机碳的调控机制,旨在为合理控制放牧强度提供理论基础。本研究以内蒙古短花针茅(Stipa breviflora)荒漠草原为研究对象,测定土壤有机碳及其活性组分含量、土壤理化性... 研究不同放牧强度对荒漠草原土壤活性有机碳的影响,了解放牧对土壤有机碳的调控机制,旨在为合理控制放牧强度提供理论基础。本研究以内蒙古短花针茅(Stipa breviflora)荒漠草原为研究对象,测定土壤有机碳及其活性组分含量、土壤理化性质和地上地下生物量及枯落物量。研究结果表明,未放牧处理荒漠草原土壤有机碳(Soil organic carbon,SOC)含量显著高于放牧处理(P<0.05);随着放牧强度的增加,土壤全氮(Total nitrogen,TN)含量逐渐降低,土壤碱解氮(Alkaline nitrogen,AN)未放牧处理均显著高于放牧处理(P<0.05),土壤容重(Bulk density,BD)、pH值逐渐升高,未放牧处理显著低于放牧处理(P<0.05),地上生物量(Aboveground biomass,AGB)、地下生物量(Belowground biomass,BGB)和枯落物(Litters,L)均随着放牧强度增加而降低。对土壤有机碳及其组分和理化性质的相关分析得出,土壤SOC含量与土壤TN,AN,AGB,L含量表现为显著正相关,土壤SOC含量与土壤BD、pH值表现为显著负相关。本研究结果表明,过度放牧会显著减少土壤有机碳。因此,建议将放牧强度维持在轻度放牧(1.54羊·hm^(-2)·a^(-1))可以有效地维持荒漠草地生产力和保护土壤有机碳。 展开更多
关键词 放牧强度 荒漠草原 土壤有机碳 生物量
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