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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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采样深度和计算方法影响保护性耕作土壤碳氮储量的评估结果 被引量:4
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作者 高奇奇 张玮 +5 位作者 马立晓 任图生 张爱平 李贵春 胡正江 杜章留 《中国农业气象》 CSCD 北大核心 2021年第1期1-12,共12页
为探讨不同年限耕作措施下土壤有机碳(SOC)和全氮(TN)在土壤剖面中的分布和累积特征,了解采样深度和计算方法对SOC和TN储量评估结果的影响,基于山东桓台(5a)和河北栾城(17a)耕作定位试验,设置翻耕(CT)、旋耕(RT)和免耕(NT)三个处理(秸... 为探讨不同年限耕作措施下土壤有机碳(SOC)和全氮(TN)在土壤剖面中的分布和累积特征,了解采样深度和计算方法对SOC和TN储量评估结果的影响,基于山东桓台(5a)和河北栾城(17a)耕作定位试验,设置翻耕(CT)、旋耕(RT)和免耕(NT)三个处理(秸秆均还田),分析土壤剖面中(桓台60cm;栾城50cm)土壤容重(ρb)、SOC和TN浓度的分布特征,并比较不同土层深度下“固定深度法(FD)”和“等效重量法(ESM)”所计算SOC和TN储量的差异。结果表明,连续多年保护性耕作后,NT处理较CT促进了SOC和TN储量在表层积累,增加了SOC和TN浓度的层化比率(SR)值。在山东桓台试验点,NT处理较CT显著增加了0-5cm土层SOC和TN储量(P<0.05),增幅分别为29%和30%,而整个土壤剖面(0-60cm)的碳氮储量分别降低8%和10%。河北栾城试验点,0-10cm土层NT和RT处理较CT分别增加SOC储量10%和14%,但在≥20cm剖面中不同耕作处理之间的碳氮储量无显著差异。由于各处理之间ρb的差异,传统FD法高估了山东桓台免耕处理SOC和TN储量,但低估了河北栾城碳氮储量。因此,为准确评估不同耕作措施下土壤碳氮固持效应,推荐在“深层采样”(≥30cm)策略基础上,利用ESM法计算其储量。保护性耕作对改善土壤质量有积极作用,但其通过土壤碳截留以缓解气候变化的潜力不应该被高估。 展开更多
关键词 保护性耕作 土壤有机碳 全氮 固定深度法 等效重量法
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东北三省土壤风蚀天数时空变化及分区评述 被引量:1
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作者 杨婉蓉 刘志娟 +3 位作者 苏正娥 高伟达 任图生 杨晓光 《中国农业气象》 CSCD 北大核心 2022年第5期327-339,共13页
基于东北三省1981-2017年气候资料,明确不同区域不同耕作阶段(全年、休耕期和播前1个月)不同等级日最大风速发生的变化规律;结合考虑降水影响下的起动风速指标,解析不同区域各阶段风蚀发生天数的时空规律,为各区域提出相适应的土壤保护... 基于东北三省1981-2017年气候资料,明确不同区域不同耕作阶段(全年、休耕期和播前1个月)不同等级日最大风速发生的变化规律;结合考虑降水影响下的起动风速指标,解析不同区域各阶段风蚀发生天数的时空规律,为各区域提出相适应的土壤保护耕作措施提供科学依据。结果表明:东北三省全年0-3级、4-6级和7级及以上日最大风速年均出现频率分别为48.5%、50.4%和1.1%,研究期内,全年、休耕期和播前1个月0-3级日最大风速出现频率均呈增加趋势,而4级及以上风速出现频率呈减少趋势。研究区域全年风蚀发生天数比例为35.0%,而播前一个月发生风蚀天数占该时期总天数的比例高于全年均值,达57.0%。大部分地区各个时期风蚀发生天数呈减少趋势。辽河平原区和三江平原区休耕期和播前1个月风蚀发生天数均较多,应重视风蚀对土壤的影响。松嫩平原区虽然休耕期土壤风蚀发生频率较低,但播前1个月风蚀发生较多,该区域应倡导免耕技术以降低土壤风蚀。 展开更多
关键词 土壤风蚀 起动风速 降水 分区评述 东北三省
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条带覆盖免耕下吉林南部玉米行间土壤水分和温度的时空动态 被引量:6
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作者 田梦 高伟达 +1 位作者 任图生 李保国 《植物营养与肥料学报》 CAS CSCD 北大核心 2022年第7期1297-1307,共11页
【目的】覆盖免耕能够减缓土壤侵蚀,提升土壤有机质含量,但在我国东北黑土区,可能会引起春季土温较低,影响玉米生长。因此,研究条带覆盖免耕(NT-SRC)技术模式下玉米行间土壤水分和温度的时空分布规律,为科学应用NT-SRC技术提供理论支撑... 【目的】覆盖免耕能够减缓土壤侵蚀,提升土壤有机质含量,但在我国东北黑土区,可能会引起春季土温较低,影响玉米生长。因此,研究条带覆盖免耕(NT-SRC)技术模式下玉米行间土壤水分和温度的时空分布规律,为科学应用NT-SRC技术提供理论支撑。【方法】玉米田间试验于2018年在吉林省南部进行,采用田间条带覆盖免耕技术模式。玉米采用宽窄行栽培,宽行行距为100 cm,秸秆全覆盖;窄行行距为40 cm,无覆盖,为玉米播种带。选择玉米行间进行原位连续监测,监测点包括玉米株下(0位点),宽行距植株10、20、30和50 cm(简称为10、20、30、50位点),窄行距植株10和20 cm(简称为–10和–20位点),每个位点土壤水分和温度监测探头埋藏5、10和20 cm 3个深度,自动连续监测土壤温度和含水量。【结果】1)NT-SRC管理下,玉米行间含水量在空间分布上呈现宽行>株下>窄行,其中含水量50位点处最高,–10位点处最低;不同监测点土壤含水量在时间尺度上的稳定性为–10<–20<10<0<20和30<50位点;土壤水分在玉米生育期内的稳定性表现为苗期>成熟期>拔节期和吐丝灌浆期。2)与窄行相比,宽行在水分较低的拔节期和吐丝灌浆期能够分别提高土壤储水量13.1%和11.1%。3)宽窄行的行间温度差异主要表现在苗期和拔节期,土壤温度由窄行20 cm处至宽行50 cm处依次降低。相较于宽行,苗期窄行的日均温提高1℃~2℃。【结论】在吉林南部地区免耕配合带状秸秆覆盖模式下,秸秆覆盖使宽行的土壤含水量和储水量在全生育期高于窄行,且土壤含水量更加稳定。无覆盖窄行提升了苗期和拔节期苗带土壤温度,对吐丝灌浆期和成熟期行间温度分布几乎无影响,缓解了吉林南部黑土区全覆盖免耕管理下玉米生长过程中的水热矛盾。 展开更多
关键词 玉米 条带覆盖免耕 土壤含水量 土壤温度 时空变异
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Soil profile characteristics of high-productivity alluvial cambisols in the North China Plain 被引量:3
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作者 LIU Hai-tao LI Bao-guo ren tu-sheng 《Journal of Integrative Agriculture》 SCIE CAS CSCD 2015年第4期765-773,共9页
The North China Plain(NCP) is one of major breadbaskets in China. Crop growth and grain yield differ significantly with spatial variations of soil properties. This study aims to identify the key soil properties in r... The North China Plain(NCP) is one of major breadbaskets in China. Crop growth and grain yield differ significantly with spatial variations of soil properties. This study aims to identify the key soil properties in relation to the grain yield for the winter wheat(Triticum aestivum L.)-maize(Zea mays L.) cropping system in a high-productivity farmland of the NCP. The field trials were conducted in three fields with different grain yield levels in Tai'an City, Shandong Province, China, during the 2009–2012 period. Consistent field management strategies were applied in the three fields. Fifty-one physical and chemical indicators of the soil profile as related to grain yield were evaluated. An approximate maximum of 17.8% annual average grain yield difference was observed in the fields during the period of 2009–2012. The soil indicators were classified into three clusters with specific functions using cluster analysis, and three key indicators were extracted from each cluster to characterize the different soil properties of three fields. The first cluster represented soil water retention capacity, and the key indicator was available soil water(ASW), which ranged from 153 to 187 mm in the 1.2 m profile and was correlated positively with grain yield. The second cluster represented soil water conductivity, as measured by saturated hydraulic conductivity(K s). The higher yield field had a greater capacity to retain topsoil water for its lower K s(1.9 cm d^–1) in the 30–70 cm soil layer as compared to the lower yield field. The third cluster represented nutrient storage and supply, as indicated by the ratio of nutrient content to silt+clay content of the top soil layer. The ratio of soil organic matter(OM), total nitrogen(TN), available P, exchangeable K+ to silt+clay content in the 0–20 cm soil layer were 19.0 g kg^–1, 1.6 g kg^–1, 94.7 mg kg^–1, 174.3 mg kg^–1 in the higher yield field, respectively, and correlated positively with the grain yield. By characterizing the differences in soil properties among fields with different yield levels, this study offers the scientific basis for increasing grain yield potential by improving the soil conditions in the NCP. 展开更多
关键词 soil quality assessment cluster analysis grain yield key soil indicators
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