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黄土高原北部生长季土壤氮素矿化对植被和地形的响应 被引量:3
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作者 刘娇 付晓莉 +3 位作者 李学章 贾小旭 邵明安 魏孝荣 《中国生态农业学报》 CSCD 北大核心 2018年第2期231-241,共11页
氮素矿化是陆地生态系统氮循环的重要过程,对氮素有效性有着重要影响。本文在黄土高原北部六道沟小流域选取退耕年限相近的油松和柠条坡地,用原位培养法测定生长季节(4—10月)不同坡位冠层下和冠层外0~10 cm和10~20 cm土层土壤氮素矿化... 氮素矿化是陆地生态系统氮循环的重要过程,对氮素有效性有着重要影响。本文在黄土高原北部六道沟小流域选取退耕年限相近的油松和柠条坡地,用原位培养法测定生长季节(4—10月)不同坡位冠层下和冠层外0~10 cm和10~20 cm土层土壤氮素矿化速率,以确定该区氮素矿化的季节动态特征和主要影响因素。结果表明,研究区生长季土壤矿质氮以铵态氮为主,其含量在0~10 cm和10~20 cm土层分别占矿质氮总量的61%和70%,并随生长季的推移而升高。油松林上坡位和中坡位土壤铵态氮显著高于下坡位土壤,柠条林不同坡位铵态氮差异不显著。土壤硝态氮和矿质氮不受坡位的影响,但与林型和采样位置有关,冠层下硝态氮在油松林与冠层外相近,在柠条林则高于冠层外。生长季土壤氮素矿化在0~10 cm土层由硝化作用引起,在10~20 cm土层则由硝化和铵化作用共同引起。铵化速率在生长季初期较高,中期较低,并受坡位、林型和采样位置的影响。土壤硝化和矿化速率在油松林不受采样位置影响,但是在柠条林则以冠层下较高。硝化和矿化速率在冠层下以下坡位土壤最高,在冠层外则以下坡位土壤最低。柠条林促进了冠层下土壤氮素的硝化和矿化过程,有利于矿质氮的积累;油松林对矿质氮和氮素矿化的影响不受采样位置影响。 展开更多
关键词 植被 坡位 矿化作用 矿质氮 采样位置
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黄土区不同土层土壤容重空间变异与模拟 被引量:26
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作者 于冬雪 贾小旭 +2 位作者 黄来明 邵明安 王娇 《土壤学报》 CAS CSCD 北大核心 2019年第1期55-64,共10页
容重(ρ_b)是土壤最基本物理性质之一,是衡量土壤质量和生产力的重要指标,也是土壤碳氮贮量估算的重要参数。为探明黄土区不同土层ρ_b的分布特征并建立预测模型,在黄土区布设243个样点,获取0~10、10~20和20~40 cm土壤ρ_b及环境因子... 容重(ρ_b)是土壤最基本物理性质之一,是衡量土壤质量和生产力的重要指标,也是土壤碳氮贮量估算的重要参数。为探明黄土区不同土层ρ_b的分布特征并建立预测模型,在黄土区布设243个样点,获取0~10、10~20和20~40 cm土壤ρ_b及环境因子,采用经典统计学与地统计学方法,分析了不同土层ρ_b的空间变异特征,并利用逐步回归和传递函数方程对ρ_b的空间分布进行了模拟。结果表明:黄土区不同土层ρ_b均为中等程度变异,ρ_b随土层深度的增加而增大。不同土层农地ρ_b最大,其次为林地和草地。0~10、10~20和20~40 cm土壤ρ_b半方差函数最佳拟合模型分别为指数模型、指数模型和球状模型,变程为22~780km。粉粒含量、坡度、海拔、多年平均降水量、气温、干燥度和土地利用是影响区域尺度黄土区ρ_b空间分布的重要因素,基于相关因子建立的传递函数模型可以解释0~40cm深度ρ_b变异的38%~52%,且预测效果优于逐步回归方程,可用于田间条件下ρ_b空间分布特征的预测。 展开更多
关键词 黄土区 容重 空间变异 土地利用 传递函数
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关中平原农田土壤水力参数空间分异与模拟 被引量:9
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作者 牛晓倩 贾小旭 +2 位作者 刘成功 邵明安 赵春雷 《水土保持学报》 CSCD 北大核心 2021年第1期198-204,共7页
土壤水力参数是土壤水分和污染物迁移等陆面过程数值模拟的重要基础参数。为探明关中平原农田土壤水力参数空间分异特征,建立空间分布预测模型,在关中平原网格布设124个样点,采集根层0-20 cm原状和扰动土壤样品,利用van Genuchten模型... 土壤水力参数是土壤水分和污染物迁移等陆面过程数值模拟的重要基础参数。为探明关中平原农田土壤水力参数空间分异特征,建立空间分布预测模型,在关中平原网格布设124个样点,采集根层0-20 cm原状和扰动土壤样品,利用van Genuchten模型拟合获取土壤水分特征曲线,获得残余含水量(θr)、饱和含水量(θs)以及系数α和n等土壤水力参数。采用经典统计学、地统计学和结构方程方法分析了θr、θs、α和n的空间变异特征及影响因子,建立了水力参数传递函数预测模型。结果表明:θr和α为强变异,θs为中等变异,n为弱变异。θr、θs、α和n半方差函数最佳拟合模型分别为球状模型、指数模型、指数模型和球状模型。θs和n具有强烈的空间依赖性,变程分别为32.7,54.3 km;θr和α具有中等程度空间依赖性,变程均为52.8 km。土壤质地、容重、pH、有机质和海拔是影响土壤水力参数空间分布的主要因子。基于土壤理化性质和海拔建立的水力参数传递函数模型具有较好的模拟效果,可用于关中地区大尺度农田生态系统土壤水力参数的模拟预测。 展开更多
关键词 关中平原 土壤水分特征曲线 水力参数 结构方程模型 传递函数模型
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华南地区草被过滤带对菜地径流、泥沙和磷阻控效果及影响因素 被引量:9
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作者 陈旭飞 刘通 +4 位作者 程炯 邵明安 孙传谆 刘平 黄斌 《水土保持研究》 CSCD 北大核心 2019年第2期377-383,共7页
通过人工模拟降雨试验,定量研究了香根草草本植被过滤带对径流、泥沙、以及全磷和溶解性磷的拦截效果。结果表明:在不同的雨强(210,120 mm/h)和不同坡度下(2°,5°),香根草过滤带能够有效拦截径流、泥沙、磷,拦截率分别可达到12... 通过人工模拟降雨试验,定量研究了香根草草本植被过滤带对径流、泥沙、以及全磷和溶解性磷的拦截效果。结果表明:在不同的雨强(210,120 mm/h)和不同坡度下(2°,5°),香根草过滤带能够有效拦截径流、泥沙、磷,拦截率分别可达到12.18%~43.11%,16.00%~70.38%,27.53%~49.35%。与120 mm/h雨强相比,210 mm/h雨强下,2种坡度下香根草过滤带小区内,径流、泥沙流失量都呈现出减少趋势,并均达到显著水平(p<0.05)。在210 mm/h雨强下,与裸坡对照相比,不同坡度处理下香根草过滤带全磷、颗粒态磷流失量都呈现出减少趋势,且二者减少程度达到显著水平,不同坡度间的流失量,存在显著差异。在不同的宽度下,香根草表现出不同的拦截效率,当宽度达到2 m时,拦截效率显著,总体上随着宽度的增加而增加。利用最优尺度回归法,对不同处理间的水文条件、坡度、带宽等影响因素进行了分析,可以发现影响植被过滤带拦截效率的主要因素包括带宽、坡度、雨强,各因子对径流、泥沙、磷流失量贡献大小分别为雨强>带宽>坡度,这表明华南地区降雨是径流、泥沙、磷流失的主要控制因子,同时,带宽对径流、泥沙、全磷的流失量也可以起到一定的积极作用。 展开更多
关键词 香根草过滤带 径流 泥沙 拦截率
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毛乌素沙地东南缘人工林樟子松根系吸水来源与影响因素 被引量:2
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作者 裴艳武 黄来明 +2 位作者 李荣磊 邵明安 张应龙 《土壤学报》 CAS CSCD 北大核心 2022年第5期1336-1348,共13页
水资源短缺是我国西北旱区沙漠化防治和植被恢复重建的主要限制因子。揭示典型治沙植物根系吸水来源及其主控因子可为该地区科学治沙和水资源高效利用提供依据。本研究选取毛乌素沙地东南缘圪丑沟小流域樟子松人工林(18—20年)为研究对... 水资源短缺是我国西北旱区沙漠化防治和植被恢复重建的主要限制因子。揭示典型治沙植物根系吸水来源及其主控因子可为该地区科学治沙和水资源高效利用提供依据。本研究选取毛乌素沙地东南缘圪丑沟小流域樟子松人工林(18—20年)为研究对象,通过定期采集和测定植物木质部水及其各种潜在水源(降水、土壤水和地下水)的氢氧同位素组成(δ^(2)H和δ^(18)O),结合多元线性混合模型研究樟子松根系吸水来源、动态变化特征及其影响因素。结果表明:监测期间(6—11月)樟子松木质部水、降水、土壤水和地下水的δ^(2)H值变化范围分别为–69.95‰~–49.25‰、–144.81‰~–6.60‰、–83.62‰~–48.57‰和–65.63‰~–53.65‰,δ^(18)O值变化范围分别为–8.77‰~–8.21‰、–18.86‰~–2.07‰、–9.45‰~–6.54‰和–9.97‰~–8.26‰。雨季(7—9月)降雨量、土壤含水量和地下水位分别高于旱季(6月,10月和11月)24.8~90.10 mm,3.36%~8.40%和5~15 cm。樟子松根系在6月主要利用深层土壤水(>90 cm)(15.40%)和地下水(70.10%),7—9月逐渐转变为以吸收浅层土壤水(<80 cm)为主(61.03%),10—11月随着降雨量减少,深层土壤水(>70 cm)和地下水对樟子松根系吸水的贡献比雨季(7—9月)分别增加5.82%~28.00%和20.64%~23.30%。毛乌素沙地樟子松人工林根系吸水来源受土壤水分供耗和地下水位季节波动的共同影响。 展开更多
关键词 毛乌素沙地 樟子松 稳定同位素 浅层地下水
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水蚀风蚀交错带退耕草坡地土壤酶活性和碳氮矿化特征 被引量:2
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作者 孔维波 石芸 +2 位作者 姚毓菲 邵明安 魏孝荣 《水土保持研究》 CSCD 北大核心 2019年第2期1-8,16,共9页
以水蚀风蚀交错带农地退耕后不同演替阶段的长芒草(Stipa bungeana)和苜蓿—铁杆蒿(Medicago sativa—Artemisia sacrorum)坡地为对象,分析了退耕坡地土壤酶活性与碳氮矿化及其空间分布特征。结果表明:(1)退耕坡地主要土壤养分含量(有... 以水蚀风蚀交错带农地退耕后不同演替阶段的长芒草(Stipa bungeana)和苜蓿—铁杆蒿(Medicago sativa—Artemisia sacrorum)坡地为对象,分析了退耕坡地土壤酶活性与碳氮矿化及其空间分布特征。结果表明:(1)退耕坡地主要土壤养分含量(有机碳、全氮和全磷)不受坡位(除苜蓿—铁杆蒿坡地的全磷含量外)影响,长芒草坡地有机碳(上、中和下坡位)和全氮含量(中和下坡位)高于苜蓿—铁杆蒿坡地。(2)随坡位的降低,长芒草坡地土壤脲酶和淀粉酶活性显著增加,蔗糖酶和碱性磷酸酶活性无显著差异。而苜蓿—铁杆蒿坡地土壤脲酶和淀粉酶活性无显著差异,蔗糖酶活性显著降低。群落类型对碱性磷酸酶活性的影响与坡位无关,对脲酶和蔗糖酶活性的影响则与坡位有关。(3)土壤有机碳矿化量和矿化速率常数在长芒草坡地显著高于苜蓿—铁杆蒿坡地,且不受坡位影响。两种群落土壤氮素矿化均由硝化作用主导,长芒草坡地土壤氮素矿化量和硝化量随坡位降低而显著增加,而苜蓿—铁杆蒿坡地则相反。(4)随苜蓿—铁杆蒿群落向长芒草群落演替,蔗糖酶和碱性磷酸酶活性空间自相关性增强,脲酶和淀粉酶活性空间自相关性减弱,但仍具有强烈空间自相关性,碳氮矿化指标的空间自相关性增强。上述结果表明:在评估退耕草坡地主要土壤过程及其空间分布时,需要考虑草地群落类型或者群落演替阶段的影响。 展开更多
关键词 水蚀风蚀交错带 退耕草坡地 土壤酶活性 碳氮矿化特征 空间自相关性
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Fractions and Bioavailability of Soil Inorganic Phosphorus in the Loess Plateau of China under Different Vegetations 被引量:6
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作者 WEI Xiaorong shao mingan +2 位作者 shao Hongbo GAO Jianlun XU Gang 《Acta Geologica Sinica(English Edition)》 SCIE CAS CSCD 2011年第1期263-270,共8页
Plants play an important role in soil phosphorus nutrition. However, the effect of plants on phosphorus nutrition in soils of the Loess Plateau of China is not well understood. This study was conducted to reveal the r... Plants play an important role in soil phosphorus nutrition. However, the effect of plants on phosphorus nutrition in soils of the Loess Plateau of China is not well understood. This study was conducted to reveal the relationships between plants and phosphorus' fractions and availability in the Loess Plateau of China. Twenty-two plant communities were surveyed and soil samples under different plant canopies were collected for the determination of soil properties and inorganic phosphorus fractionation. The results showed that Leguminosae and Lilaceae reduced pH and increased organic matter, cation exchange capacity, total and Olsen phosphorus in soils under their canopies, while Labiatae and Rosaceae increased pH and decreased organic matter, cation exchange capacity, total and Olsen phosphorus in soils under their canopies. The contents of Ca2P, CasP, AI-P and Fe-P were highly related with soil Oisen phosphorus. They were all higher in soils under Leguminosae and Lilaceae and lower in softs under Labiatae and Rosaceae. The results of this study indicate that Leguminosae and Lilaceae improved phosphorus nutrition in soils, yet Labiatae and Rosaceae impeded the improvement of phosphorus nutrition in soils under their canopies, which will be of more help to instruct vegetation restoration in the region and provide information for soil development. 展开更多
关键词 BIOAVAILABILITY FRACTION inorganic phosphorus VEGETATION soil development Loess Plateau
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水蚀风蚀交错带草地土壤碳氮组分对柠条的响应特征
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作者 朱寒松 李学章 +2 位作者 贾小旭 邵明安 魏孝荣 《水土保持研究》 CSCD 北大核心 2018年第5期29-35,共7页
采用相对密度分组法研究了水蚀风蚀交错带不同年限草地和相邻柠条林地0—40cm土层土壤碳氮组分分布特征,旨在揭示研究区草地土壤碳氮组分对柠条的响应特征。研究结果显示:草地转变为柠条林后,土壤重组有机碳和全氮含量变化很小(分别介于... 采用相对密度分组法研究了水蚀风蚀交错带不同年限草地和相邻柠条林地0—40cm土层土壤碳氮组分分布特征,旨在揭示研究区草地土壤碳氮组分对柠条的响应特征。研究结果显示:草地转变为柠条林后,土壤重组有机碳和全氮含量变化很小(分别介于-0.19~0.06g/kg和-0.001~0.017g/kg),而轻组有机碳和全氮含量变化较大,并且随年限和土层的不同而异。25年柠条林地土壤有机碳和全氮在0—40cm土层的储量分别增加了10.94 Mg C/hm^2,0.07 Mg N/hm^2,而轻组有机碳和全氮分别增加了2.41 Mg C/hm^2,0.11 Mg N/hm^2;40年柠条林0—40cm土层土壤轻组有机碳降低了4.54 Mg C/hm^2重组有机碳和总有机碳增加了6.26,1.72Mg C/hm^2;而土壤全氮、轻组和重组全氮储量分别降低了0.73,0.44,0.29 Mg N/hm^2。这些结果表明草地转变为柠条林后,土壤有机碳和全氮的变化分别由重组有机碳和轻组全氮引起。 展开更多
关键词 水蚀风蚀交错带 草地 柠条 有机碳组分 氮组分 不同生长年限
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Roles of ABA Signal Transduction during Higher Plant Seed Development and Germination 被引量:5
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作者 shao Hongbo Liang Zongsuo shao mingan 《Forestry Studies in China》 CAS 2003年第4期45-53,共9页
ABA is one of the 5 phytohormones in higher plants, which is also the most important hormone that regulates higher plants in response to environmental stress, by ABA signal transduction. Understanding ABA signal trans... ABA is one of the 5 phytohormones in higher plants, which is also the most important hormone that regulates higher plants in response to environmental stress, by ABA signal transduction. Understanding ABA signal transduction at the molecular level is crucial to biology and ecology, and rational breeding complied with corresponding eco-environmental changes. Great advancements have taken place over the past 10 years by application of the Arabidopsis experimental system. Many components involved in ABA signal transduction have been isolated and identified and a clear overall picture of gene expression and control for this transduction has become an accepted fact. On the basis of the work in our laboratory, in conjunction with the data available at the moment, the authors have attempted to integrate ABA signal transduction pathways into a common one and give some insights into the relationship between ABA signal transduction and other hormone signal transduction pathways, with an emphasis upon the ABA signal transduction during higher plant seed development. A future challenge in this field is that different experimental systems are applied and various receptors and genes need to be characterized through the utilization of microarray chips. 展开更多
关键词 molecular biology ABA signal transduction ABA-responsive genes seed development environmental stresses
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沙地长柄扁桃研究进展 被引量:5
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作者 孙树臣 邵明安 +2 位作者 翟胜 田晓飞 张清心 《林业科技通讯》 2020年第4期20-26,共7页
回顾了长柄扁桃(Amygdalus predunculata Pall.)在种质资源与分布、种苗繁育与引种栽培、植物形态学与生理学特性和综合效益等领域取得的重要进展。针对长柄扁桃当前的研究现状及进展,提出应加强长柄扁桃林地蒸散耗水规律及水量平衡过... 回顾了长柄扁桃(Amygdalus predunculata Pall.)在种质资源与分布、种苗繁育与引种栽培、植物形态学与生理学特性和综合效益等领域取得的重要进展。针对长柄扁桃当前的研究现状及进展,提出应加强长柄扁桃林地蒸散耗水规律及水量平衡过程、适宜栽植密度及田间优化管理等3个方面的研究。以期为加快推进长柄扁桃研究,服务于区域生态环境建设及经济发展提供理论依据。 展开更多
关键词 沙地 长柄扁桃 Amygdalus predunculata Pall. 生态效益 水量平衡
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Characteristics of Dried Soil Layers Under Apple Orchards of Different Ages and Their Applications in Soil Water Managements on the Loess Plateau of China 被引量:21
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作者 WANG Yunqiang shao mingan +1 位作者 LIU Zhipeng ZHANG Chencheng 《Pedosphere》 SCIE CAS CSCD 2015年第4期546-554,共9页
Negative soil water balance(i.e., water input < water output) can lead to soil desiccation and subsequently the occurrence of a dried soil layer(DSL). The DSLs are generally studied at a specific sampling depth(e.g... Negative soil water balance(i.e., water input < water output) can lead to soil desiccation and subsequently the occurrence of a dried soil layer(DSL). The DSLs are generally studied at a specific sampling depth(e.g., 500 cm), and the actual extent of DSLs remains unknown due to the challenge of collecting deep soil samples. To investigate the characteristics of actual DSLs under different ages of apple orchards and ascertain the optimal age of apple orchards for avoiding/controlling the formation of DSLs, soil samples were collected to a depth of 1 800 cm under apple orchards of different ages in Changwu on the Loess Plateau of China. As the ages increased, soil water content(SWC) and mean SWC in DSLs showed an overall decreasing trend, whereas while DSL thickness and the quantity of water deficit(QWD) in DSLs demonstrated an increasing trend. The DSL was the thickest(1 600 cm) under the 17-year-old orchard, the forming velocity of DSL thickness was the highest at the apple tree growth stage of 9–17 years(168 cm year-1), and the highest increasing velocity of QWD(-181 mm year-1) was also observed at this stage. The thickness of DSL was significantly correlated with growth age and root depth of apple trees(r > 0.88), whereas the QWD and mean SWC in DSLs were found to have no correlation with them. The optimal age of apple orchards for avoiding/controlling the formation of DSLs was about 9 years. This information provided pertinent references for the management of deep water resources by controlling the growth age of plants. 展开更多
关键词 土壤水分管理 中国黄土高原 生长年龄 土壤干层 苹果园 特征和 土壤干燥化 应用
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Evapotranspiration and its main controlling mechanism over the desert riparian forests in the lower Tarim River Basin 被引量:14
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作者 YUAN GuoFu LUO Yi +2 位作者 shao mingan ZHANG Pei ZHU XuChao 《Science China Earth Sciences》 SCIE EI CAS CSCD 2015年第6期1032-1042,共11页
Evapotranspiration(ET) and its controlling mechanism over the desert riparian forests in arid regions are the important scientific basis for the water resources managements of the lower reaches of the inland rivers of... Evapotranspiration(ET) and its controlling mechanism over the desert riparian forests in arid regions are the important scientific basis for the water resources managements of the lower reaches of the inland rivers of China. Nearly three years of continuous measurements of surface ET, soil water content at different depths and groundwater table over a typical Tamarix spp. stand and a typical Populus euphratica stand were conducted in the lower reach of the Tarim River. The ET seasonal trends in the growing season were controlled by plant phenology, and ET in non-growing season was weak. The diurnal variations of ET resulting from the comprehensive effects of all atmospheric factors were significantly related with reference ET. The spatial pattern of ET was determined by vegetation LAI, more vegetation coverage, more ET amount. Groundwater is the water source of surface ET, and the soil water in shallow layers hardly took part in the water exchange in the groundwatersoil-plant-air system. The temporal processes of ET over the Tamarix stand and the Populus stand were similar, but the water consumption of the well-grown Populus euphratica was higher than that of the well-grown Tamarix spp. Further analysis indicates that plant transpiration accounts for most of the surface ET, with soil evaporation weak and negligible; groundwater table is a crucial factor influencing ET over the desert riparian forests, groundwater influences the processes and amounts of ET by controlling the growth and spatial distribution of desert riparian forests; quantifying the water stress of desert riparian forests using groundwater table is more appropriate, rather than soil water content. Based on the understanding of ET and water movements in the groundwater-soil-plant-air system, a generalized framework expressing the water cycling and its key controlling mechanism in the lower reaches of the inland rivers of China is described, and a simple model to estimate water requirements of the desert riparian forests is presented. 展开更多
关键词 荒漠河岸林 塔里木河流域 控制生长 蒸散量 机制 土壤含水量 地下水位 植被覆盖度
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