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推求土壤水分运动参数的简单入渗法──Ⅱ.实验验证 被引量:36
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作者 邵明安 王全九 robert horton 《土壤学报》 CAS CSCD 北大核心 2000年第2期217-224,共8页
预报土壤中水分流动需要的土壤导水特性可通过观测水平土柱的入渗过程来确定,这一观测过程的分析是基于对Richards方程求积分解。土壤水分特征曲线中的参数由观测的水平立柱的特征湿润长度和吸力来确定,非饱和土壤导水率由已确定的特... 预报土壤中水分流动需要的土壤导水特性可通过观测水平土柱的入渗过程来确定,这一观测过程的分析是基于对Richards方程求积分解。土壤水分特征曲线中的参数由观测的水平立柱的特征湿润长度和吸力来确定,非饱和土壤导水率由已确定的特征曲线中的参数和测定的饱和导水率导出。供试土壤有三种,它们的质地从砂壤到粘壤。由这种方法所确定的这三种土壤的水分特征曲线与实测的特征曲线符合良好,所确定的砂壤的非他和导水率与实测值的比较令人满意。利用数值法和积分法分别计算了土壤含水量剖面,计算结果吻合良好,说明了这种方法的合理性。 展开更多
关键词 简单入渗法 土壤异水特性 水平土柱实验
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新疆参考作物腾发量多元回归模型及空间分布 被引量:4
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作者 廖轶群 李毅 +1 位作者 robert horton 崔晨风 《排灌机械工程学报》 EI 北大核心 2012年第1期117-124,共8页
利用新疆境内42个气象站的多年气象资料,应用Penman-Monteith公式计算得到各站逐日和逐月尺度下的ET0值,应用多元统计回归分析得到相应的ET0与主要气象要素的回归方程,作为各地区计算ET0的经验公式.结合ArcGIS软件的空间分析功能,将各... 利用新疆境内42个气象站的多年气象资料,应用Penman-Monteith公式计算得到各站逐日和逐月尺度下的ET0值,应用多元统计回归分析得到相应的ET0与主要气象要素的回归方程,作为各地区计算ET0的经验公式.结合ArcGIS软件的空间分析功能,将各站回归方程的系数进行插值得出整个新疆地区ET0经验公式回归参数的空间分布图.结果表明,逐日和逐月尺度下,区域内的ET0空间分布差异显著,南部明显高于北部.回归所得的经验方程用来估算各地的ET0值是合理可靠的.回归所得的经验方程较Penman-Monteith公式简化得多,且具有一定精度,因此有一定的推广价值和应用前景.对于无气象资料地区,通过查图得出参数值,即可推算该区域特定时间尺度下的ET0值. 展开更多
关键词 参考作物腾发量 PENMAN-MONTEITH公式 日尺度 月尺度 空间分布
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斥水土壤的水力参数及水平吸渗规律 被引量:3
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作者 刘世宾 李毅 robert horton 《排灌机械工程学报》 EI 北大核心 2013年第11期1000-1006,共7页
为了对不同斥水程度土壤的水力性质进行分析,对比了van Genuchten和Brooks-Corey模型对于不同斥水程度下的塿土、砂姜黑土、盐碱土和砂土的适用性;进行了一维水平吸渗试验,分别运用Philip模型和Kostiakov公式对入渗规律进行了模拟,并分... 为了对不同斥水程度土壤的水力性质进行分析,对比了van Genuchten和Brooks-Corey模型对于不同斥水程度下的塿土、砂姜黑土、盐碱土和砂土的适用性;进行了一维水平吸渗试验,分别运用Philip模型和Kostiakov公式对入渗规律进行了模拟,并分析了吸渗率和斥水持续时间的关系;采用水平吸渗法推求了土壤非饱和扩散率,并用指数函数拟合了非饱和扩散率和体积含水率的关系.结果表明:van Genuchten和Brooks-Corey模型对亲水和斥水土壤均具有较好的适用性;斥水性土壤的累积入渗量随时间变化曲线在一定时刻发生转折,未转折前Kostiakov公式的模拟结果比Philip模型好;当斥水时间大于40 s时,吸渗率的变化趋于稳定并在0~0.1 cm/min0.5内变化;非饱和扩散率和体积含水率关系的模拟可采用指数关系,且其对亲水性土壤的模拟效果优于斥水性土壤.斥水土壤的水力参数与亲水土壤的有明显差别,且表现出特殊性. 展开更多
关键词 斥水土壤 水分特征曲线 非饱和扩散率 水平吸渗 湿润锋
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基于土壤LFUHF频段介电特性的FDR测量频率研究 被引量:3
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作者 许景辉 马孝义 +1 位作者 Sally D Logsdon robert horton 《农业机械学报》 EI CAS CSCD 北大核心 2013年第7期67-72,共6页
土壤介电特性是影响FDR传感器测量土壤含水量精度和适应性的重要物理参数。为了确定28 mm长、10 mm间距的7探针FDR传感器理想频率,通过矢量网络分析仪对4种不同土壤的LF-UHF频段(1 MHz~3 GHz)散射参数进行了测量,通过Logsdon和Laird模... 土壤介电特性是影响FDR传感器测量土壤含水量精度和适应性的重要物理参数。为了确定28 mm长、10 mm间距的7探针FDR传感器理想频率,通过矢量网络分析仪对4种不同土壤的LF-UHF频段(1 MHz~3 GHz)散射参数进行了测量,通过Logsdon和Laird模型变换,使用Matlab进行了4种土壤表观介电常数的计算和绘制。通过土壤介电频谱分析,研究了土壤极化机理,分析了土壤介电特性与频率的关系,确定了FDR传感器的工作频段为44~398 MHz,考虑到温度对极化的影响,其最佳工作频段为62~110 MHz,其中75 MHz是其工作的最佳频率。此频率下土壤介电值仅对土壤含水量敏感,是消除温度等因素对FDR传感器影响的理想频率。 展开更多
关键词 土壤含水量 介电特性 FDR 测量频率
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Using Copula functions to predict climatic change impacts on floods in river source regions 被引量:1
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作者 Ting-Xing CHEN Hai-Shen LYU +5 位作者 robert horton Yong-Hua ZHU Ren-Sheng CHEN Ming-Yue SUN Ming-Wen LIU Yu LIN 《Advances in Climate Change Research》 SCIE CSCD 2024年第3期406-418,共13页
Flood frequency in river source regions is significantly affected by rainfall and snowmelt as part of climatic changes.A traditional univariate flood frequency analysis cannot reflect the complexity of floods,and when... Flood frequency in river source regions is significantly affected by rainfall and snowmelt as part of climatic changes.A traditional univariate flood frequency analysis cannot reflect the complexity of floods,and when used in isolation,it can only underestimate flood risk.For effective flood prevention and mitigation,it is essential to consider the combined effects of precipitation and snowmelt.Copula functions can effectively quantify the joint distribution relationship between floods and their associated variables without restrictions on their distribution characteristics.This study uses copula functions to consider a multivariate probability distribution model of flood peak flow(Q)with cumulative snowmelt(CSm)and cumulative precipitation(CPr)for the Hutubi River basin located in northern Xinjiang,China.The joint frequencies of rainfall and snowmelt floods are predicted using copula models based on the Coupled Model Intercomparison Project Phase 6 data.The results show that Q has a significant positive correlation with 24-d CSm(r=0.559,p=0.002)and 23-d CPr(r=0.965,p<0.05).Flood frequency will increase in the future,and mid-(2050e2074)and long-term(2075e2099)floods will be more severe than those in the near-term(2025e2049).The probability of flood occurrence is higher under the SSP2-4.5 and SSP1-2.6 scenarios than under SSP5-8.5.Precipitation during the historical period(1990e2014)led to extreme floods,and increasing future precipitation trends are found to be insignificant.Snowmelt increases with rising temperatures and occurs earlier than estimated,leading to an earlier flood period in the basin and more frequent snowmelt floods.The Q under the joint return period is larger than that during the same univariate return period.This difference indicates that neglecting the interaction between precipitation and snowmelt for floods leads to an underestimation of the flood risk(with underestimations ranging from 0.3%to 22%).The underestimations decrease with an increase in the return period.The joint risks of rainfall or snowmelt according to various flood periods should be considered for rivers with multi-source runoff recharge in flood control design.This study reveals the joint impact of precipitation and snowmelt on extreme floods under climate change in river source regions.This study also provides a scientific basis for regional flood prevention and mitigation strategies,as well as for the rational allocation of water resources. 展开更多
关键词 Climate change Flood frequency COPULA CMIP6 River source regions
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Humic acid transport in saturated porous media:Influence of flow velocity and influent concentration 被引量:3
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作者 Xiaorong Wei Mingan Shao +1 位作者 Lina Du robert horton 《Journal of Environmental Sciences》 SCIE EI CAS CSCD 2014年第12期2554-2561,共8页
Understanding the transport of humic acids(HAs) in porous media can provide important and practical evidence needed for accurate prediction of organic/inorganic contaminant transport in different environmental media... Understanding the transport of humic acids(HAs) in porous media can provide important and practical evidence needed for accurate prediction of organic/inorganic contaminant transport in different environmental media and interfaces. A series of column transport experiments was conducted to evaluate the transport of HA in different porous media at different flow velocities and influent HA concentrations. Low flow velocity and influent concentration were found to favor the adsorption and deposition of HA onto sand grains packed into columns and to give higher equilibrium distribution coefficients and deposition rate coefficients, which resulted in an increased fraction of HA being retained in columns.Consequently, retardation factors were increased and the transport of HA through the columns was delayed. These results suggest that the transport of HA in porous media is primarily controlled by the attachment of HA to the solid matrix. Accordingly, this attachment should be considered in studies of HA behavior in porous media. 展开更多
关键词 ATTACHMENT Flow velocity Humic acid Initial concentration Porous media TRANSPORT
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