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Estimation of evapotranspiration from artificial forest in mountainous areas of western Loess Plateau based on HYDRUS-1D model 被引量:2
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作者 LU Rui ZHANG Mingjun +4 位作者 ZHANG Yu QIANG Yuquan CHE Cunwei SUN Meiling WANG Shengjie 《Journal of Arid Land》 SCIE CSCD 2024年第12期1664-1685,共22页
Evapotranspiration is the most important expenditure item in the water balance of terrestrial ecosystems,and accurate evapotranspiration modeling is of great significance for hydrological,ecological,agricultural,and w... Evapotranspiration is the most important expenditure item in the water balance of terrestrial ecosystems,and accurate evapotranspiration modeling is of great significance for hydrological,ecological,agricultural,and water resource management.Artificial forests are an important means of vegetation restoration in the western Loess Plateau,and accurate estimates of their evapotranspiration are essential to the management and development of water use strategies for artificial forests.This study estimated the soil moisture and evapotranspiration based on the HYDRUS-1D model for the artificial Platycladus orientalis(L.)Franco forest in western mountains of Loess Plateau,China from 20 April to 31 October,2023.Moreover,the influence factors were identified by combining the correlation coefficient method and the principal component analysis(PCA)method.The results showed that HYDRUS-1D model had strong applicability in portraying hydrological processes in this area and revealed soil water surplus from 20 April to 31 October,2023.The soil water accumulation was 49.64 mm;the potential evapotranspiration(ET_(p))was 809.67 mm,which was divided into potential evaporation(E_(p);95.07 mm)and potential transpiration(T_(p);714.60 mm);and the actual evapotranspiration(ET_(a))was 580.27 mm,which was divided into actual evaporation(E_(a);68.27 mm)and actual transpiration(T_(a);512.00 mm).From April to October 2023,the ET_(p),E_(p),T_(p),ET_(a),E_(a),and T_(a) first increased and then decreased on both monthly and daily scales,exhibiting a single-peak type trend.The average ratio of T_(a)/ET_(a) was 0.88,signifying that evapotranspiration mainly stemmed from transpiration in this area.The ratio of ET_(a)/ET_(p) was 0.72,indicating that this artificial forest suffered from obvious drought stress.The ET_(p) was significantly positively correlated with ET_(a),and the R^(2) values on the monthly and daily scales were 0.9696 and 0.9635(P<0.05),respectively.Furthermore,ET_(a) was significantly positively correlated with temperature,solar radiation,and wind speed,and negatively correlated with relative humidity and precipitation(P<0.05);and temperature exhibited the highest correlation with ET_(a).Thus,ET_(p) and temperature were the decisive contributors to ET_(a) in this area.The findings provide an effective method for simulating regional evapotranspiration and theoretical reference for water management of artificial forests,and deepen understanding of effects of each influence factors on ET_(a) in arid areas. 展开更多
关键词 potential evapotranspiration actual evapotranspiration EVAPORATION TRANSPIRATION HYDRUS-1d model Loess Plateau soil water content
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Validation of 1D model for methane/air/Pt combustion in stagnation flow
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作者 刘明候 邢丹 +1 位作者 陆雨洲 朱会元 《Applied Mathematics and Mechanics(English Edition)》 SCIE EI 2013年第5期577-588,共12页
A 2D model is built on the package of FLUENT to study the effects of radial aspect ratio (R/W), length-to-width ratio (L/W), strain rate (SR), and buoyancy (Ri=Gr/Re^2) on the validation of the simplified 1D m... A 2D model is built on the package of FLUENT to study the effects of radial aspect ratio (R/W), length-to-width ratio (L/W), strain rate (SR), and buoyancy (Ri=Gr/Re^2) on the validation of the simplified 1D model. In the present 2D model, the methane/air homogeneous reaction mechanism of Peters and the methane/air/platinum heterogeneous reaction mechanism of Deutschmann are applied. By comparison between the 1D and 2D numerical results, it is found that the validation of 1D model is highly related with the catalytic stagnation reactor configuration. For length-to-width ratio L/W = 1 configuration, 1D laminar model is applicable when the radial aspect ratio R/W 〉 0.4. For R/W = 0.6, the reactor exhibited 1D characteristics when L/W 〈 1. Compared with the temperature and species profiles, the velocity distribution along the axis is more sensitive to the change of radial aspect ratio and length-to-width ratio. With increasing of the strain rate, the flame front goes closer to the catalytic wall surface and the difference between the 1D and 2D results decreases. For a valid 1D simulation, it is recommended that the strain rate should be convection can be neglected when Ri〈 5. greater than 20 s^-1. The effects of natural 展开更多
关键词 stagnation flow catalytic reaction validation of 1d model
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基于1D-CNN的稻谷石墨烯远红外干燥模型及含水率在线预测 被引量:1
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作者 王逸凡 井世亮 +3 位作者 夏宇 Nuhu Jibril 赵海瑞 陈坤杰 《南京农业大学学报》 北大核心 2025年第2期488-497,共10页
[目的]为实现远红外稻谷干燥过程中水分比的精准预测,提出了一种基于1D-CNN(one-dimensional convolutional neural network)的稻谷干燥水分比预测模型,实现对干燥过程中稻谷含水率在线预测。[方法]将稻谷初始含水率调到统一标准后,在... [目的]为实现远红外稻谷干燥过程中水分比的精准预测,提出了一种基于1D-CNN(one-dimensional convolutional neural network)的稻谷干燥水分比预测模型,实现对干燥过程中稻谷含水率在线预测。[方法]将稻谷初始含水率调到统一标准后,在自制的石墨烯远红外干燥试验台进行不同温度的干燥试验,每隔2 min采集1组包括干燥温湿度等8个工艺参数数据,经标准化处理后构成数据集。然后以8个工艺参数为输入,水分比为输出,构建1D-CNN干燥模型,通过训练确定模型参数,最后对模型进行验证并与6种经典薄层干燥模型及4种典型机器学习干燥模型进行比较。[结果]试验结果表明,所提出的1D-CNN干燥模型能够很好描述干燥过程中水分比的变化情况,决定系数R^(2)、均方根误差(root mean square error, RMSE)和平均绝对误差(mean absolute error, MAE)分别达到0.993 1、0.018 9、0.012 1;含水率预测的MAE和平均相对误差(mean relative error, MRE)分别为0.143 2%和0.007 8%,明显优于其他对比的干燥模型。[结论]所提出的1D-CNN干燥模型能够准确预测稻谷干燥过程中含水率变化,完全满足含水率在线检测需求。 展开更多
关键词 稻谷 1d-CNN模型 石墨烯远红外干燥 含水率在线预测
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An Implicit Coupled 1D/2D Model for Unsteady Subcritical Flow in Channel Networks and Embayment
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作者 GENG Yan-fen WANG Zhi-li 《China Ocean Engineering》 SCIE EI CSCD 2020年第1期110-118,共9页
In this study, 1D and 2D shallow-water models were coupled to simulate unsteady flow in channel networks and embayment. The 1D model solved the 1D shallow-water equations (St. Venant) using the Preissmann box method a... In this study, 1D and 2D shallow-water models were coupled to simulate unsteady flow in channel networks and embayment. The 1D model solved the 1D shallow-water equations (St. Venant) using the Preissmann box method and targeted long narrow reaches of the river networks, while the 2D model targeted broad channels and embayment and solved the 2D shallow-water equations using a semi-implicit scheme applied to an unstructured grid of triangular cells. The 1D and 2D models were solved simultaneously by building a matrix for the free surface elevation at every 1D junction and 2D cell center. Velocities were then computed explicitly based on the results at the previous time step and the updated water level. The originality of the scheme arose from a novel coupling method. The results showed that the coupled 1D/2D model produced identical results as the full 2D model in classical to benchmark problems with considerable savings in computational effort. Application of the model to the Pearl River Estuary in southern China showed that complex patterns of tidal wave propagation could be efficiently modeled. 展开更多
关键词 1d river network model 2D unstructured model full coupling model Pearl River Delta
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基于Hydrus-1D模型的宁夏河东沙地固定沙丘花棒林土壤水分动态模拟
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作者 张维福 展秀丽 +2 位作者 马思怡 张呈春 马晓霞 《水土保持通报》 北大核心 2025年第5期267-276,325,共11页
[目的]探究宁夏河东沙地固定沙丘花棒林土壤水分的变化规律,为该区沙漠化持续治理和防沙治沙效果评价提供科学参考。[方法]利用Hydrus-1D模型,模拟0—150 cm土壤剖面的土壤水分垂直分布和时间变化特征,并采用决定系数R2、均方根误差RMS... [目的]探究宁夏河东沙地固定沙丘花棒林土壤水分的变化规律,为该区沙漠化持续治理和防沙治沙效果评价提供科学参考。[方法]利用Hydrus-1D模型,模拟0—150 cm土壤剖面的土壤水分垂直分布和时间变化特征,并采用决定系数R2、均方根误差RMSE和相对误差RE评价了模型在宁夏河东沙地的适用性。[结果]①降雨入渗表现出阈值依赖特征:降雨量小于2.2 mm时,入渗深度小于5 cm,降雨量介于3.6~8.2 mm时,入渗深度介于5~15 cm;降雨量介于10.8~22.8 mm时,入渗深度介于15~30 cm;②利用Hydrus-1D模型模拟花棒林地不同深度土壤含水量总体模拟效果较好,模拟阶段和验证阶段决定系数分别为0.756和0.773,均方根误差分别为0.071%和0.064%,相对误差分别为0.030%,0.032%;表层5 cm和深层125 cm土壤含水量拟合精度不高,15,30,50,80 cm土壤含水量模拟效果较好,土层决定系数范围为0.571~0.849,均方根误差为0.0001%~0.042%。[结论]不同降雨事件下的入渗效果有所差异,总体上降雨入渗的深度随着降雨量的增加而增加。Hydrus-1D模型模拟的土壤含水量与实测值吻合度较高,并证明该模型适用于模拟宁夏河东沙地土壤剖面的含水量。 展开更多
关键词 土壤水分 HYDRUS-1d模型 入渗深度 适用性 宁夏河东沙地
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Simulation of the Hydrodynamic Functioning of the Cavally River Using a Coupled 1D-2D Model in the Ity Area (Zouan-Hounien in Côte d’Ivoire)
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作者 Affoué Berthe Yao Kouao Armand Anoh +2 位作者 Loukou Alexis Brou Menouan Wilfried Goli Lazare Kouakou Kouassi 《Open Journal of Modern Hydrology》 2021年第4期75-84,共10页
In recent years, the Cavally River has been subject to multiple activities, <span style="font-family:;" "="">including the construction of diversion channels and a bridge that makes it v... In recent years, the Cavally River has been subject to multiple activities, <span style="font-family:;" "="">including the construction of diversion channels and a bridge that makes it vulnerable to flooding. In order to assess the impact of these hydraulic structures on the <span>river hydrodynamic functioning, a 1D-2D model was realized. The</span> implementation of the 1D-2D model consisted </span><span style="font-family:;" "="">of </span><span style="font-family:;" "="">first </span><span style="font-family:;" "="">running</span><span style="font-family:;" "=""> </span><span style="font-family:;" "="">the 1D model, then the 2D model, and finally in coupling them. The 1D-2D model was designed with <span>the 1988 flood hydrograph, a Manning’s coefficient of 0.052 m<sup>1/3</sup>/s for the </span>minor bed and 0.06 m<sup>1/3</sup>/s for the major bed. The results of the hydraulic model show that the velocities are almost identical to those of the Cavally in natural operation. The values of the velocities are included between 0.4 m/s and 1.3 m/s at the level of the minor bed of the river and between 0.06 m/s and 0.71 m/s at the level of the floodplains. The average water level for flood propagation is 262.37 ± 0.44 m before construction of the structures and 262.23 ± <span>0.85 m after construction of the structures. The 0.41 m reduction in water</span> level due to the diversion canal and bridge is negligible compared to the total fluctuations of the Cavally River, which vary from 6 to 7 m over the year.</span> 展开更多
关键词 Ity Mines 1d-2D modeling FLOODING Cavally River Côte d’Ivoire
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Fine-scale damage assessment of urban flooding based on the 1D/2D coupled hydrodynamic model 被引量:1
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作者 Boliang Dong Junqiang Xia +1 位作者 Qijie Li Xiaojie Wang 《River》 2023年第4期403-420,共18页
Due to the high population density and economic property in urban environments,urban flooding can result in substantial economic losses.However,accurate urban flood modeling and assessing the associated damages are ch... Due to the high population density and economic property in urban environments,urban flooding can result in substantial economic losses.However,accurate urban flood modeling and assessing the associated damages are challenging due to complex urban layouts and rugged topography.Furthermore,the rapid development of urban underground spaces has introduced additional complexities.To address the demanding need for accurate flood modeling and damage assessment in cities,a fine-scale flood damage assessment method was proposed in this study,based on the 1D/2D coupled hydrodynamic model,which can not only assess the flood damage on the ground surface but also evaluate the flood loss in underground spaces.Taking the Gangxi drainage area in Wuhan City,China as a case,this study extensively discussed the flood inundation processes on the ground surface as well as in the buildings and underground spaces,under different rainfall scenarios with the return period ranging from 2 to 200 years.Based on the high spatial-temporal hydrodynamic simulations,the flood damage degrees were evaluated for the buildings and underground spaces with different industry types.The results indicated that the inundation of buildings and underground spaces in densely built cities cannot be neglected in urban flood modeling.Buildings with public service attributes can have a higher flood damage degree,as compared with other types of buildings and underground spaces. 展开更多
关键词 1d/2D coupled modeling flood damage assessment underground spaces urban flooding
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Temperature Distributions in Single Cell of Polymer Electrolyte Fuel Cell Simulated by an 1D Multi-plate Heat-Transfer Model and a 3D Numerical Simulation Model
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作者 Akira Nishimura Masashi Baba +3 位作者 Kotaro Osada Takenori Fukuoka MasafumiHirota Eric Hu 《Journal of Energy and Power Engineering》 2015年第8期687-704,共18页
The purpose of this study is to verify an 1D multi-plate heat-transfer model estimating the temperature distribution on the interface between polymer electrolyte membrane and catalyst layer at cathode in single cell o... The purpose of this study is to verify an 1D multi-plate heat-transfer model estimating the temperature distribution on the interface between polymer electrolyte membrane and catalyst layer at cathode in single cell of polymer electrolyte fuel cell, which is named as reaction surface in this study, with a 3D numerical simulation model solving many governing equations on the coupling phenomena in the cell. The results from both models/simulations agreed well. The effects of initial operation temperature, flow rate, and relative humidity of supply gas on temperature distribution on the reaction surface were also investigated. It was found in both 1D and 3D simulations that, the temperature rise (i.e., Treact-Tini) of the reaction surface from initial operation temperature at 70℃ was higher than that at 80℃ irrespective of flow rate of supply gas. The effect of relative humidity of supply gas on Treact- Tini near the inlet of the cell was small. Compared to the previous studies conducted under the similar operation conditions, the Treact - Tini calculated by 1D multi-plate heat-transfer model in this study as well as numerical simulation using 3D model was reasonable. 展开更多
关键词 Polymer electrolyte fuel cell 1d multi-plate heat-transfer model 3D numerical simulation model temperaturedistribution.
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A deterministic distributed modeling approach of Mediterranean water-cycle assessment,application in the Var catchment,France
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作者 Siyuan Chang Zhengmiao Li +2 位作者 Xinyi Lian Philippe Gourbesville Qiang Ma 《River》 2025年第3期297-310,共14页
Characterized by special morphologic,geographic,hydrologic,and societal behaviors,the water resources management of the Mediterranean catchment often shows a higher level of complexity including security issues of wat... Characterized by special morphologic,geographic,hydrologic,and societal behaviors,the water resources management of the Mediterranean catchment often shows a higher level of complexity including security issues of water supply,inundation risks,and environment management under the perspective of climate change.To have a comprehensive understanding of the Mediterranean water-cycle system,a deterministic distributed hydrologic modeling approach has been developed and presented in this study based on an application in the Var catchment(2800 km^(2))located at the French Mediterranean region.A 1D and 2D coupled model of MIKE SHE and MIKE 11 has been set up under a series of hypotheses to represent the whole hydrologic and hydrodynamic processes including rainfall-runoff,snow-melting,channel flow,overland flow,and the water exchange between land surface and unsaturated/saturated zones.The developed model was first calibrated with 4 years daily records from 2008 to 2011,then to be validated and further run within hourly time interval to produce detailed representation of the catchment water-cycle from 2012 to 2014.The deterministic distributed modeling approach presented in this study is able to represent its complicated water-cycle and used for supporting the decision‐making process of the water resources management of the catchment. 展开更多
关键词 1d/2D coupled model distributed hydrological model flood management Mediterranean catchment
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基于1D-CNN和Transformer模型的道岔健康状态预测
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作者 陈俊竹 陈光武 +1 位作者 石建强 邢东峰 《北京交通大学学报》 北大核心 2025年第3期33-43,共11页
针对目前铁路道岔故障率高、维护效率低、健康状态难以预测等问题,以S700K型道岔转辙机为研究对象,提出一种基于一维卷积神经网络(One-dimensional Convolutional Neural Net-work,1D-CNN)和Transformer模型结合的道岔健康状态预测方法... 针对目前铁路道岔故障率高、维护效率低、健康状态难以预测等问题,以S700K型道岔转辙机为研究对象,提出一种基于一维卷积神经网络(One-dimensional Convolutional Neural Net-work,1D-CNN)和Transformer模型结合的道岔健康状态预测方法.首先,采用1D-CNN对原始数据进行特征提取,训练得到10组特征;然后,通过特征评价选择其中最能反映道岔健康状态的5组特征,利用它们与道岔功率曲线的健康标签值共同进行Transformer模型训练,得到预测的健康指数;最后,为评估道岔转辙设备的健康状态,采用Fisher最优分割算法对健康阶段进行划分,确定最优健康阶数为3,并针对不同健康阶段的维护工作给出指导性意见.研究结果表明:1D-CNN和Transformer模型的结合具有较为突出的预测效果与泛化能力,Transformer模型较门控循环单元(Gated Recurrent Unit,GRU)、长短期记忆网络(Long Short-Term Memory,LSTM)等常用模型在处理长时间序列数据时具有更好的表现,采用所提组合模型能得到更为准确的道岔健康状态预测结果,其平均绝对误差(Mean Absolute Error,MAE)、均方根误差(Root Mean Square Error,RMSE)较1D-CNN和LSTM的组合模型分别减小31.2%、30.5%. 展开更多
关键词 铁路道岔 一维卷积神经网络 Transformer模型 健康状态预测 Fisher最优分割
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HYDRUS-1D模型对河套灌区不同灌施情景下氮素迁移的模拟 被引量:47
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作者 郝芳华 孙雯 +3 位作者 曾阿妍 李鹏 张嘉勋 岳勇 《环境科学学报》 CAS CSCD 北大核心 2008年第5期853-858,共6页
选取河套灌区五原建丰的典型土壤,应用HYDRUS-1D模型对不同灌溉强度、不同表施浓度以及将表施改为灌施3类情景下土壤氮元素的迁移进行了动态模拟,研究了灌溉和施肥对河套灌区典型区域土壤氮元素迁移的影响.结果表明,灌水强度小于0.10 cm... 选取河套灌区五原建丰的典型土壤,应用HYDRUS-1D模型对不同灌溉强度、不同表施浓度以及将表施改为灌施3类情景下土壤氮元素的迁移进行了动态模拟,研究了灌溉和施肥对河套灌区典型区域土壤氮元素迁移的影响.结果表明,灌水强度小于0.10 cm.h-1时,铵态氮与硝态氮累积流出通量变化极为缓慢;强度大于0.14 cm.h-1时,累积流出通量急剧攀升,表明氮元素大量向土层深层流失.铵态氮表施浓度的变化对氮素的迁移几乎没有影响.保持相同的施肥量,灌施情景对铵态氮迁移几乎无影响,但表施换为灌施后硝态氮下渗浓度增加47%,更易于向深层渗漏. 展开更多
关键词 河套灌区 HYDRUS-1d模型 硝态氮 铵态氮 迁移
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应用HYDRUS-1D模型模拟农田土壤水渗漏及硝态氮淋失特征 被引量:30
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作者 毕经伟 张佳宝 +2 位作者 陈效民 朱安宁 冯杰 《农村生态环境》 CSSCI CSCD 北大核心 2004年第2期28-32,共5页
在定位试验基础上,应用HYDRUS-1D模型对黄淮海平原典型土壤(黄潮土)中土壤水渗漏及硝态氮淋失动态进行了模拟分析。结果表明:在传统水氮管理模式下,黄潮土2m土体深处的土壤水渗漏和硝态氮淋失非常严重,2个轮作期内,土壤水渗漏总量占地... 在定位试验基础上,应用HYDRUS-1D模型对黄淮海平原典型土壤(黄潮土)中土壤水渗漏及硝态氮淋失动态进行了模拟分析。结果表明:在传统水氮管理模式下,黄潮土2m土体深处的土壤水渗漏和硝态氮淋失非常严重,2个轮作期内,土壤水渗漏总量占地表总入水量的23.7%,硝态氮淋失总量占总输入N量的15.9%,冬小麦生长季的硝态氮淋失量大于夏玉米生长季;改良灌溉和改良施肥模式下产生的硝态氮淋失量比传统灌溉和传统施肥模式减少74.7%,节约灌溉水211.5mm、节省施N423.5kg·hm-2。 展开更多
关键词 HYDRUS-1d模型 土壤水 渗漏 硝态氮 淋失
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Hydrus-1D模型在田间水循环规律分析中的应用及改进 被引量:50
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作者 马欢 杨大文 +2 位作者 雷慧闽 蔡建峰 楠田哲也 《农业工程学报》 EI CAS CSCD 北大核心 2011年第3期6-12,共7页
为分析农田水分运移规律,以华北平原位山引黄灌区典型田间为研究对象,应用Hydrus-1D模型连续模拟了2006-2009年的田间水分运移过程。对模型中表面阻抗的计算方法进行了改进,从而改善了蒸散发的模拟结果,与涡度相关系统的实测蒸散发数据... 为分析农田水分运移规律,以华北平原位山引黄灌区典型田间为研究对象,应用Hydrus-1D模型连续模拟了2006-2009年的田间水分运移过程。对模型中表面阻抗的计算方法进行了改进,从而改善了蒸散发的模拟结果,与涡度相关系统的实测蒸散发数据对比表明了改进的合理性。对蒸散发的分析表明,对于种植季节性作物的农田,叶面积指数(leafarea index,LAI)是影响蒸散发季节变化过程的重要因素,而气象条件主要决定其在较短时间尺度(如一周)内的波动。与时域反射仪(time domain reflectometry,TDR)实测土壤含水率的对比表明,模型对土壤含水率的模拟精度较高。水量平衡分析结果表明,降雨和灌溉的80%由蒸散发消耗,在汛期农田通过排水发生田间渗漏损失。 展开更多
关键词 蒸发 蒸腾 模型 HYDRUS-1d模型 位山灌区 水量平衡
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基于Hydrus-1D模型的大安灌区旱田灌溉入渗补给研究 被引量:15
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作者 卞建民 李育松 +1 位作者 胡昱欣 李宏亮 《干旱地区农业研究》 CSCD 北大核心 2014年第2期191-195,共5页
以吉林省大安灌区为研究对象,在野外调查和资料收集的基础上,借助Hydrus-1D模型,模拟分析了旱田(玉米地)灌溉条件下地下水入渗补给过程。结果表明:模拟期间蒸散发动态变化较大,蒸腾量约为蒸发量的2.18倍,玉米生育期内,土壤水分蒸腾损失... 以吉林省大安灌区为研究对象,在野外调查和资料收集的基础上,借助Hydrus-1D模型,模拟分析了旱田(玉米地)灌溉条件下地下水入渗补给过程。结果表明:模拟期间蒸散发动态变化较大,蒸腾量约为蒸发量的2.18倍,玉米生育期内,土壤水分蒸腾损失约占蒸散发消耗的79.74%,蒸散发在作物生长旺季以蒸腾为主,其它时段则以蒸发为主;旱田灌溉条件下,降水灌溉大量入渗形成土壤水,土壤水与地下水发生双向的、动态的水量频繁交换,模拟中地下水入渗补给量约为33.63 mm,入渗比为5.21%,其与研究区细密的包气带介质岩性有关。研究成果可为进一步开展旱田灌溉合理方案的制定提供科学依据。 展开更多
关键词 大安灌区 Hydrus -1d 模型 旱田灌溉 入渗补给
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应用HYDRUS-1D模型评价土壤水资源量 被引量:20
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作者 王水献 周金龙 +1 位作者 余芳 董新光 《水土保持研究》 CSCD 北大核心 2005年第2期36-38,共3页
利用焉耆盆地典型试验区观测资料,以土壤水动力学原理为基础,建立起浅埋区(埋深≤2m)植被覆盖条件下田间土壤水分数学模型,对典型试验区土壤水资源量补给项、排泄项和消耗项进行计算与评价,评价结果表明:地下水资源和土壤水资源转化十... 利用焉耆盆地典型试验区观测资料,以土壤水动力学原理为基础,建立起浅埋区(埋深≤2m)植被覆盖条件下田间土壤水分数学模型,对典型试验区土壤水资源量补给项、排泄项和消耗项进行计算与评价,评价结果表明:地下水资源和土壤水资源转化十分频繁,水量交换是双向的、动态的;在浅埋区土壤水库调蓄能力较弱,造成部分灌溉水的渗漏。 展开更多
关键词 HYDRUS-1d模型 土壤水资源量 焉耆盆地
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基于Hydrus-1D模型的毛乌素沙地杨柴(Hedysarum laeve)灌木林土壤含水量模拟 被引量:7
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作者 洪光宇 王晓江 +9 位作者 刘铁山 海龙 吴振廷 胡尔查 高孝威 杨海峰 李卓凡 李梓豪 斯琴 王乐军 《中国沙漠》 CSCD 北大核心 2022年第6期233-242,共10页
在干旱半干旱区植被恢复与重建过程中,土壤储水量会发生明显变化。土壤水分是限制植被生长的主要因子,运用数学模拟的方法研究植被建设后土壤水分变化特征,能更快预测土壤水分的亏缺情况。本研究选用Hydrus-1D模型,模拟毛乌素沙地典型... 在干旱半干旱区植被恢复与重建过程中,土壤储水量会发生明显变化。土壤水分是限制植被生长的主要因子,运用数学模拟的方法研究植被建设后土壤水分变化特征,能更快预测土壤水分的亏缺情况。本研究选用Hydrus-1D模型,模拟毛乌素沙地典型灌木林杨柴(Hedysarum laeve)群落的土壤水分空间和时间变化,评估Hydrus-1D模型在毛乌素沙地杨柴人工林地的适用性。以杨柴生长季为研究期,通过调查的各项实测值带入Hydrus-1D模型并对参数进行优化后模拟杨柴群落土壤水分时间和空间的变化过程,利用同时间段Watchdog土壤水分监测仪连续监测的不同土层土壤含水量数据作为对照值验证其模拟值的适用性。结果表明:研究区飞播杨柴灌木林地不同深度土壤水分实测值与模拟值的决定系数0.55—0.78,均方根误差0.005%—0.0143%,实测值与模拟值具有较好的一致性,说明Hydrus-1D模型适用于模拟毛乌素沙地杨柴灌木林土壤剖面的水分变化。 展开更多
关键词 毛乌素沙地 杨柴灌木林 土壤水分 HYDRUS-1d模型 适用性
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利用Hydrus-1D模拟分层土壤剖面的水流运动 被引量:5
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作者 董晓华 刘潇钧 +3 位作者 彭涛 姚着喜 郭梁锋 刘璇璇 《安徽农业科学》 CAS 2016年第4期29-31,共3页
[目的]研究分层土壤水分运移规律,进行水分运移的数值模拟。[方法]利用Hydrus-1D软件,通过设定不同上下边界条件,进行分层土壤的水分运移模拟。[结果]利用Hydrus-1D软件可以模拟到水分运移中观测点的水头、含水量及土壤上表层流量的随... [目的]研究分层土壤水分运移规律,进行水分运移的数值模拟。[方法]利用Hydrus-1D软件,通过设定不同上下边界条件,进行分层土壤的水分运移模拟。[结果]利用Hydrus-1D软件可以模拟到水分运移中观测点的水头、含水量及土壤上表层流量的随时间的变化规律。[结论]水分运移中的地面边界流量、水头和含水量与降雨量的变化直接相关,科学可靠的气象数据对水分运移的模拟非常重要。 展开更多
关键词 HYDRUS-1d 水分运移 数值模拟
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DRAINMOD和HYDRUS-1D模型对水稻控制灌排条件下农田水位的模拟 被引量:3
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作者 俞双恩 李倩倩 +4 位作者 陈凯文 张梦婷 王梅 王煜 刘子鑫 《河海大学学报(自然科学版)》 CAS CSCD 北大核心 2020年第1期46-52,共7页
为研究水稻控制灌排条件下农田水位的变化,根据2017年的水稻测坑种植试验资料,率定DRAINMOD模型和HYDRUS-1D模型参数,以相关系数、平均偏差及纳什效率系数为评价标准,通过比较2018年农田水位模拟值与实测值的吻合程度,分析2种模型模拟... 为研究水稻控制灌排条件下农田水位的变化,根据2017年的水稻测坑种植试验资料,率定DRAINMOD模型和HYDRUS-1D模型参数,以相关系数、平均偏差及纳什效率系数为评价标准,通过比较2018年农田水位模拟值与实测值的吻合程度,分析2种模型模拟稻田干湿交替条件下农田水位的可靠性。结果表明:DRAINMOD模型和HYDRUS-1D模型的模拟结果均能较好地反映农田水位的实际变化情况,模拟值与实测值的相关系数分别为0.778和0.849,平均偏差分别为2.051 cm和1.809 cm,纳什效率系数分别为0.509和0.360,且2个模型模拟结果没有显著差别;DRAINMOD模型和HYDRUS-1D模型均可用于模拟水稻控制灌排条件下农田水位变化,为稻田水分运移研究提供方便可行的方法。 展开更多
关键词 控制灌排 测坑试验 水稻种植 农田水位 DRAINMOD模型 HYDRUS-1d模型
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One-dimensional breakdown voltage model of SOI RESURF lateral power device based on lateral linearly graded approximation
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作者 张珺 郭宇锋 +4 位作者 徐跃 林宏 杨慧 洪洋 姚佳飞 《Chinese Physics B》 SCIE EI CAS CSCD 2015年第2期474-479,共6页
A novel one-dimensional(1D) analytical model is proposed for quantifying the breakdown voltage of a reduced surface field(RESURF) lateral power device fabricated on silicon on an insulator(SOI) substrate.We assu... A novel one-dimensional(1D) analytical model is proposed for quantifying the breakdown voltage of a reduced surface field(RESURF) lateral power device fabricated on silicon on an insulator(SOI) substrate.We assume that the charges in the depletion region contribute to the lateral PN junctions along the diagonal of the area shared by the lateral and vertical depletion regions.Based on the assumption,the lateral PN junction behaves as a linearly graded junction,thus resulting in a reduced surface electric field and high breakdown voltage.Using the proposed model,the breakdown voltage as a function of device parameters is investigated and compared with the numerical simulation by the TCAD tools.The analytical results are shown to be in fair agreement with the numerical results.Finally,a new RESURF criterion is derived which offers a useful scheme to optimize the structure parameters.This simple 1D model provides a clear physical insight into the RESURF effect and a new explanation on the improvement in breakdown voltage in an SOI RESURF device. 展开更多
关键词 SOI RESURE breakdown voltage 1d model
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基于Hydrus-1D模型的科尔沁沙地沙丘-草甸相间区土壤水分动态模拟 被引量:13
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作者 王宇祥 刘廷玺 +4 位作者 段利民 童新 王冠丽 李东方 王海英 《中国沙漠》 CSCD 北大核心 2020年第2期195-205,共11页
土壤水分是干旱半干旱地区生态环境的主要限制性因子,研究科尔沁沙地流动沙丘和草甸地土壤水分动态规律有助于荒漠化地区的生态恢复和保护。以2018年5月25日至10月31日为研究期,利用土壤各项实测参数和气象数据,评价Hydrus-1D模型在科... 土壤水分是干旱半干旱地区生态环境的主要限制性因子,研究科尔沁沙地流动沙丘和草甸地土壤水分动态规律有助于荒漠化地区的生态恢复和保护。以2018年5月25日至10月31日为研究期,利用土壤各项实测参数和气象数据,评价Hydrus-1D模型在科尔沁沙地的适用性,并揭示科尔沁沙丘-草甸相间区土壤水分分布特征,重点分析研究区流动沙丘200 cm剖面和草甸地80 cm剖面土壤水分的动态规律。结果表明:研究区典型土地类型流动沙丘和草甸地土壤水分模拟值和实测值的决定系数均高于0.76,均方根误差0.01~0.02 cm3·cm-3;在土壤剖面上具有明显的分层结构,流动沙丘分为3层,即0~20 cm为干沙层,20~120 cm为活跃层,120~200 cm为稳定层,其中40 cm土壤水分波动性最大;草甸地分为2层,即0~40 cm为活跃层,40~80 cm为稳定层,主要受降雨、蒸散发和地下水位影响;流动沙丘和草甸地降雨与表层土壤水分呈极显著相关,降雨量与地下水位变化仅草甸地呈显著正相关;在整个研究期内,流动沙丘土壤水分储量变化量为12.6 mm,土壤实际蒸发量为105.9 mm,200 cm深层渗漏量为173.9 mm,占总降雨量的59.5%;草甸地土壤水分储量变化量为8 mm,80 cm深层渗漏量为-27.2 mm(地下水补给量),土壤实际蒸发量为67 mm,植被蒸腾量为244 mm,地表径流量为0 mm。 展开更多
关键词 流动沙丘 草甸地 HYDRUS-1d模型 适用性
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