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科尔沁沙地21种植物水分提升作用的实证检验 被引量:6
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作者 阿拉木萨 周丽芳 《北京林业大学学报》 CAS CSCD 北大核心 2011年第1期70-77,共8页
对科尔沁沙地21种植物开展了水分提升作用检测和发生特点研究。试验采用上下层土壤隔离的自制栽植箱,通过控制上、下层土壤水分含量的方法检测植物水分提升作用。结果表明:有19个参试物种观测到水分提升作用,水分提升作用可能是沙生植... 对科尔沁沙地21种植物开展了水分提升作用检测和发生特点研究。试验采用上下层土壤隔离的自制栽植箱,通过控制上、下层土壤水分含量的方法检测植物水分提升作用。结果表明:有19个参试物种观测到水分提升作用,水分提升作用可能是沙生植物适应干旱环境的普遍特性;植物水分提升作用在00:00-06:00时段内发生频率和提升数量较高;不同物种间水分提升能力存在差异,本研究首次采用每克根系生物量(干质量)24h可产生的水分提升数量作为比较植物水分提升能力的单位,其数值变化范围为4.86~325.62g/g之间,平均为72.9g/g。综合比较认为,乌丹蒿、万年蒿、牧马豆和雾冰藜具有较强的水分提升能力。浅层土壤干旱程度与累计水分提升数量在统计学分析上并未表现出明显的相关性。利用植物水分提升能力改善固沙植被区浅层土壤水分环境条件,对提高半干旱区人工固沙植被的稳定性具有重要意义。 展开更多
关键词 沙生植物 水分提升 土壤水分再分配 科尔沁沙地
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干旱区内陆河流域荒漠河岸林群落生态过程与水文机制研究 被引量:49
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作者 李卫红 郝兴明 +2 位作者 覃新闻 陈亚宁 黄湘 《中国沙漠》 CSCD 北大核心 2008年第6期1113-1117,共5页
干旱区内陆河流域生态水文过程研究已成为当今地理学、生态学研究的焦点,是开展生态恢复研究的重要内容。塔里木河下游断流河道的生态恢复是以沿自然河道生态输水为主要形式的,因此,有必要加深对塔里木河下游荒漠河岸林群落生态过程与... 干旱区内陆河流域生态水文过程研究已成为当今地理学、生态学研究的焦点,是开展生态恢复研究的重要内容。塔里木河下游断流河道的生态恢复是以沿自然河道生态输水为主要形式的,因此,有必要加深对塔里木河下游荒漠河岸林群落生态过程与水文机制的认识。在对塔里木河下游荒漠河岸林植被生态退化及其退化原因分析的基础上,综述了塔里木河下游典型植物生态水位的研究进展,阐述了植物适宜生态水位、胁迫地下水位和临界地下水位研究的阶段性成果,并进一步展望了未来研究的焦点问题。指出了群落生态水位、植被群落与土壤水分、盐分异质性的关系,提出植物水分利用机制是群落生态过程与水文机制研究的核心问题。 展开更多
关键词 生态过程 生态水位 土壤盐分异质性 土壤水分再分配 塔里木河下游
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Characterising Vertical Redistribution on Irrigated Furrows in the Tukulu Soil
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作者 Sabelo Sicelo Wesley Mavimbela Leon Daniel van Rensburg Alain Cloot 《Journal of Agricultural Science and Technology(A)》 2013年第7期542-560,共19页
Subsurface soil water redistribution on the South African Tukulu, also referred as the Cutanic Luvisols in other countries, was evaluated following single run irrigation (20, 40, 80 and 160 L/min inflow rates) in 90... Subsurface soil water redistribution on the South African Tukulu, also referred as the Cutanic Luvisols in other countries, was evaluated following single run irrigation (20, 40, 80 and 160 L/min inflow rates) in 90 m furrows. Changes in soil water content (SWC) at three horizons were monitored using neutron water meter. Measurements were made every 10 m starting 5 m from the furrow inlet for 455 h. HYDRUS-2D software was used to estimate soil hydraulic parameters through inverse optimization algorithms for redistribution at the inlet, midpoint and furrow end. Optimized model parameters compared with initial estimates recorded satisfactory agreement between measured and predicted soil water content, despite spatial variability. Effective hydraulic conductivity (Keff) for 0-600 mm and 0-850 mm profile flow domains demonstrated linearity with SWC although inconsistencies under field conditions were inevitable. The underlying layer restricted gravity and augmented redistribution with Keff assuming a steeper gradient than normal. Conversion of KCff and soil water content into a ratio assisted in quantifying rate of redistribution at 0-600 mm and 0-850 mm profile depth. Vertical redistribution was found to be limited within the upper 600 mm depth thus providing the opportunity to develop furrow irrigation with confidence that water productivity is optimized. 展开更多
关键词 Soil water redistribution inflow rates effective unsaturated hydraulic conductivity infiltrated depth HYDRUS-2D.
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Impacts of hydraulic redistribution on eco-hydrological cycles: A case study over the Amazon basin 被引量:3
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作者 Yuanyuan WANG Binghao JIA Zhenghui XIE 《Science China Earth Sciences》 SCIE EI CAS CSCD 2018年第9期1330-1340,共11页
Hydraulic redistribution(HR)refers to the process of soil water transport through the low-resistance pathway provided by plant roots.It has been observed in field studies and proposed to be one of the processes that e... Hydraulic redistribution(HR)refers to the process of soil water transport through the low-resistance pathway provided by plant roots.It has been observed in field studies and proposed to be one of the processes that enable plants to resist water limitations.However,most land-surface models(LSMs)currently do not include this underground root process.In this study,a HR scheme was incorporated into the Community Land Model version 4.5(CLM4.5)to investigate the effect of HR on the eco-hydrological cycle.Two paired numerical simulations(with and without the new HR scheme)were conducted for the Tapajos National Forest km83(BRSa3)site and the Amazon.Simulations for the BRSa3 site in the Amazon showed that HR during the wet season was small,<0.1 mm day^(–1),transferring water from shallow wet layers to deep dry layers at night;however,HR in the dry season was more obvious,up to 0.3 mm day^(–1),transferring water from deep wet layers to shallow dry layers at night.By incorporating HR into CLM4.5,the new model increased gross primary production(GPP)and evapotranspiration(ET)by 10%and 15%,respectively,at the BRSa3 site,partly overcoming the underestimation.For the Amazon,regional analysis also revealed that vegetation responses(including GPP and ET)to seasonal drought and the severe drought of 2005 were better captured with the HR scheme incorporated. 展开更多
关键词 Land-surface model CLM4.5 Hydraulic redistribution Gross primary production EVAPOTRANSPIRATION
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