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Soil Aggregate Stability and Aggregate-Associated Carbon Under Different Tillage Systems in the North China Plain 被引量:21
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作者 DU Zhang-liu REN Tu-sheng +2 位作者 HU Chun-sheng ZHANG Qing-zhong Humberto Blanco-Canqui 《Journal of Integrative Agriculture》 SCIE CAS CSCD 2013年第11期2114-2123,共10页
The inlfuences of tillage systems on soil carbon (C) stocks have been studied extensively, but the distribution of soil C within aggregate fractions is not well understood. The objective of this study was to determi... The inlfuences of tillage systems on soil carbon (C) stocks have been studied extensively, but the distribution of soil C within aggregate fractions is not well understood. The objective of this study was to determine the inlfuences of various tillage systems on soil aggregation and aggregate-associated C under wheat (Triticum aestivum L.) and corn (Zea mays L.) double cropping systems in the North China Plain. The experiment was established in 2001, including four treatments:moldboard plow (MP) with residue (MP+R) and without residue (MP-R), rotary tillage with residue (RT), and no-till with residue (NT). In 2007 soil samples were collected from the 0-5, 5-10, and 10-20 cm depths, and were separated into four aggregate-size classes (〉2 000, 250-2 000, 53-250, and〈53 μm) by wet-sieving method. Aggregate-associated C was determined, and the relationships between total soil C concentration and aggregation-size fractions were examined. The results showed that NT and RT treatments signiifcantly increased the proportion of macroaggregate fractions (〉2 000 and 250-2 000 μm) compared with the MP-R and MP+R treatments. Averaged across all depths, mean weight diameters of aggregates (MWD) in NT and RT were 47 and 20% higher than that in MP+R. The concentration of bulk soil organic C was positively correlated with MWD (r=0.98; P=0.024) and macroaggregate fraction (r=0.96; P=0.036) in the 0-5 cm depth. In the 0-20 cm depth, comparing with MP+R, total C occluded in the〉2 000 μm fraction was increased by 9 and 6%under NT and RT, respectively. We conclude that adoption of conservation tillage system, especially no-till, can increase soil macro-aggregation and total C accumulation in macroaggregates, which may improve soil C sequestration in the intensive agricultural region of the North China Plain. 展开更多
关键词 tillage systems aggregate stability aggregate-associated c
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东北黑土水稳性团聚体及其结合碳分布特征 被引量:30
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作者 梁爱珍 张晓平 +2 位作者 申艳 李文凤 杨学明 《应用生态学报》 CAS CSCD 北大核心 2008年第5期1052-1057,共6页
以东北黑土区32对自然和耕作黑土为研究对象,对比研究了两种土壤水稳性团聚体及其结合碳的分布特征.结果表明:自然土壤0~30cm水稳性大团聚体(>0.25mm)质量分数及其结合碳均高于微团聚体;随着土层深度的增加,大团聚体及其结合碳逐渐... 以东北黑土区32对自然和耕作黑土为研究对象,对比研究了两种土壤水稳性团聚体及其结合碳的分布特征.结果表明:自然土壤0~30cm水稳性大团聚体(>0.25mm)质量分数及其结合碳均高于微团聚体;随着土层深度的增加,大团聚体及其结合碳逐渐降低,而微团聚体(<0.25mm)及其结合碳显著增加(P<0.01).耕作土壤团聚体分布特征与自然土壤相反,与自然土壤相比,耕作土壤大团聚体数量及其结合碳急剧降低,且>1mm的大团聚体降低幅度远大于其他粒级团聚体.自然土壤大团聚体质量分数与土壤有机碳(SOC)存在明显的正相关关系(P<0.01),尤其是>1mm大团聚体;耕作土壤>1mm大团聚体质量分数与土壤总SOC相关不显著;自然与耕作土壤总SOC与各级团聚体结合碳呈极显著正相关(P<0.01).与自然土壤相比,耕作土壤大团聚体结合碳明显降低,而微团聚体结合碳增加了37.1%,总SOC含量下降了29.5%,表明大团聚体在总SOC变化中起主要作用.水稳性大团聚体对管理措施响应迅速,可以作为评价农业管理措施转变对土壤肥力和土壤质量影响的指标. 展开更多
关键词 水稳性团聚体 团聚体结合碳 大团聚体 黑土
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Short-Term Effect of Nitrogen Intensification on Aggregate Size Distribution, Microbial Biomass and Enzyme Activities in a Semi-Arid Soil Under Different Crop Types 被引量:2
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作者 Rajasekaran MURUGAN V. R. Ramakrishna PARAMA +2 位作者 Beate MADAN R. MUTHURAJU Bernard LUDWIG 《Pedosphere》 SCIE CAS CSCD 2019年第4期483-491,共9页
There is a lack of quantitative assessments available on the effect of agricultural intensification on soil aggregate distribution and microbial properties. Here, we investigated how short-term nitrogen(N) intensifica... There is a lack of quantitative assessments available on the effect of agricultural intensification on soil aggregate distribution and microbial properties. Here, we investigated how short-term nitrogen(N) intensification induced changes in aggregate size distribution and microbial properties in a soil of a hot moist semi-arid region(Bangalore, India). We hypothesised that N intensification would increase the accumulation of macroaggregates > 2 mm and soil microbial biomass and activity, and that the specific crop plant sowed would influence the level of this increase. In November 2016, surface(0–10 cm) and subsurface(10–20 cm) soil samples were taken from three N fertilisation treatments, low N(50 kg N ha-1), medium N(75 and 100 kg N ha-1 for finger millet and maize, respectively),and high N(100 and 150 kg N ha-1 for finger millet and maize, respectively). Distribution of water-stable aggregate concentrations,carbon(C) and N dynamics within aggregate size class, and soil microbial biomass and activity were evaluated. The high-N treatment significantly increased the concentration of large macroaggregates in the subsurface soil of the maize crop treatment, presumably due to an increased C input from root growth. Different N fertilisation levels did not significantly affect C and N concentrations in different aggregate size classes or the bulk soil. High-N applications significantly increased dehydrogenase activity in both the surface soil and the subsurface soil and urease activity in the surface soil, likely because of increased accumulation of enzymes stabilised by soil colloids in dry soils. Dehydrogenase activity was significantly affected by the type of crop, but urease activity not. Overall, our results showed that high N application rates alter large macroaggregates and enzyme activities in surface and subsurface soils through an increased aboveground and corresponding belowground biomass input in the maize crop. 展开更多
关键词 AGRIcULTURAL INTENSIFIcATION biomass input c and N dynamics large macroaggregate microaggregate N application small macroaggregate water-stable AGGREGATES
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