共查询到19条相似文献，搜索用时 109 毫秒
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在珠江三角洲潮流量巡测资料的分析基础上，探讨了提高潮流量测验精度的方法。采用代表线流速、潮位、潮位涨落率等多要素进行相关的方法，提高了潮流量代表线流速定线精度，不但能降低潮流量测验强度和成本，而且还能提高测验、整编质量和经济效益。 相似文献
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根据田庄台站2000年1月潮位资料,对潮水位及潮流量的数据进行统计分析,可知潮流量及潮水位具有周期性涨落变化,二者随时间不断变化而变化,其流速、流向也相应随时间发生变化。认识、掌握潮流量的变化规律对指导测验时机、资料分析及城市排污、泄污有一定意义。 相似文献
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本文以枝城站流量测验资料为研究对象,从辐射杆测船定位和GPS测船定位两个资料系列分析,得出在特殊河床中因测深定位对流量造成误差的影响. 相似文献
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长江河口段徐六泾水文站潮流量整编代表线法研究 总被引：4，自引：1，他引：3
长江河口段河道宽阔,断面几何形状复杂,水流往复流动,水力条件变化复杂,潮流量测验及整编一直是难题。随着多普勒剖面流速仪（ADCP）在技术上日益完善以及无线通讯技术的快速发展,解决长江河口段徐六泾水文站潮流量测验及整编问题具备了切实可行的技术条件。经过近两年的努力,根据代表线法测流原理,采用浮标ADCP结合平台ADCP的测流系统,徐六泾水文站成功地实现了断面流量、流速的实时监测,潮流量整编成果达到了规范要求。 相似文献
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粗颗粒悬移质测验误差分析 总被引：2，自引：0，他引：2
本文根据流速与含沙量分布,研究了悬移质积点法对粗颗粒含沙量测验误差.首先指出无论从输沙率还是从悬浮高度看,粗颗粒悬移质集中于河底,致使水文测验中的一些测验方法(如一点法、二点法、三点法等)带有较大的误差.进而分析了各种测法对粗颗粒的相对误差,并且随着颗粒变粗,误差愈来愈大,以致不能接受.这种情况在水库下游河道冲刷过程中,会在一定程度上出现,必须重视研究和调整测验方法.最后通过与长江委水文局在沙市及监利两水文站试验结果对比,证明本文理论上的分析是可信的. 相似文献
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通过介绍野外数字化测图的方法和步骤,对两种测图方法在地物点、地形点施测中产生的误差进行分析比较,坐标法测图误差主要来源:测站点误差、视距(或测距)误差、展点误差及高程正中误差;数字化测图误差来源:点位中误差、平面位置中误差、高程中误差.通过对比得出野外数字化测图具有成图精度高,野外工作量少,工作效率高,可任意制作不同比例尺地形图,容易保存等优点;野外数字化测图是工程地形测量发展方向,必将取代传统的测图方式. 相似文献
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Rory D. Henderson Frederick D. Day-Lewis Elena Abarca Charles F. Harvey Hanan N. Karam Lanbo Liu John W. Lane Jr. 《Hydrogeology Journal》2010,18(1):173-185
Electrical resistivity imaging has been used in coastal settings to characterize fresh submarine groundwater discharge and the position of the freshwater/salt-water interface because of the relation of bulk electrical conductivity to pore-fluid conductivity, which in turn is a function of salinity. Interpretation of tomograms for hydrologic processes is complicated by inversion artifacts, uncertainty associated with survey geometry limitations, measurement errors, and choice of regularization method. Variation of seawater over tidal cycles poses unique challenges for inversion. The capabilities and limitations of resistivity imaging are presented for characterizing the distribution of freshwater and saltwater beneath a beach. The experimental results provide new insight into fresh submarine groundwater discharge at Waquoit Bay National Estuarine Research Reserve, East Falmouth, Massachusetts (USA). Tomograms from the experimental data indicate that fresh submarine groundwater discharge may shut down at high tide, whereas temperature data indicate that the discharge continues throughout the tidal cycle. Sensitivity analysis and synthetic modeling provide insight into resolving power in the presence of a time-varying saline water layer. In general, vertical electrodes and cross-hole measurements improve the inversion results regardless of the tidal level, whereas the resolution of surface arrays is more sensitive to time-varying saline water layer. 相似文献
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针对现有水位流量关系线型物理机制不强及流量估算不确定性来源考虑不充分问题,以北江流域石角水文站为例,推导该测站水位流量关系,基于BaRatin模型评估流量测量误差及率定样本选取对估算流量不确定性的影响。发现河槽控制宽浅矩形断面水位流量关系为幂函数,其系数可用糙率、河宽、比降表达,指数为定值5/3;考虑流量测量误差后高水估算流量总不确定性减小32%;率定数据增加1倍、3倍,高水估算流量总不确定性减小12%、34%。结果表明:① 水位流量关系模型建立方法可推广至多类型测站;② 高水测量误差对率定精度影响较大,建议提高高水流量测量精度;③ 现有实测水位与流量数据存在信息冗余,主要存在于低水数据中,本方法可减少率定数据使用,降低整编成本。 相似文献
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针对现有水位流量关系线型物理机制不强及流量估算不确定性来源考虑不充分问题,以北江流域石角水文站为例,推导该测站水位流量关系,基于BaRatin模型评估流量测量误差及率定样本选取对估算流量不确定性的影响。发现河槽控制宽浅矩形断面水位流量关系为幂函数,其系数可用糙率、河宽、比降表达,指数为定值5/3;考虑流量测量误差后高水估算流量总不确定性减小32%;率定数据增加1倍、3倍,高水估算流量总不确定性减小12%、34%。结果表明:①水位流量关系模型建立方法可推广至多类型测站;②高水测量误差对率定精度影响较大,建议提高高水流量测量精度;③现有实测水位与流量数据存在信息冗余,主要存在于低水数据中,本方法可减少率定数据使用,降低整编成本。 相似文献
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Charles T. Roman 《Estuaries and Coasts》1984,7(3):259-264
Water volume discharge estimates were made at a sample cross-section of the Canary Creek salt marsh (Lewes, Delaware). To account for cross-sectional velocity variations, a dense spatial array of current meters was used. Simultaneous measurements were taken at hourly intervals over three complete tidal cycles. A practical method is presented whereby instantaneous average cross-sectional velocity, instantaneous cross-sectional discharge and tidal cycle discharge can be estimated from a dense current meter array, orideal data set. Based on theseideal estimates, it is shown that a simplified spatial array can be used to estimate water discharges within acceptable error limits. Instantaneous cross-sectional discharges and total tidal cycle discharges were estimated with uncertainties of ±11% and ±7%, respectively. To minimize errors when estimating material exchange between salt marshes and adjacent waters, it is suggested that a comprehensive assessment of cross-sectional lateral current velocity variations be conducted. 相似文献
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目前,测流不确定度通过误差试验或通过经验数值来确定,但这些方式存在着工作量大或不确定估计不足等局限性。为解决此问题,对基于实测数据和统计理论的插值方差估计法在不同测流条件下进行了验证,选取白河、襄阳和沙洋3个流量站进行了实测数据的不确定度分析,同时对白河站进行了Monte Carlo试验,比较插值方差估计法得到的不确定度与真实误差的差异。结果表明,插值方差估计法能较好地反映水位变化的影响,插值方差估计法所得到的不确定度与真实测流误差的相关系数达0.64,与断面水位变化的Spearman相关系数达0.79,高、中水位情况下插值方差估计法的不确定度估计结果较为合理,低水位情况下偏高。 相似文献
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The groundwater tidal prism is defined as the volume of water that inundates a porous medium, forced by one tidal oscillation in surface water. The pressure gradient that generates the prism acts on the subterranean estuary. Analytical models for the groundwater tidal prism and associated benthic flux are presented. The prism and flux are shown to be directly proportional to porosity, tidal amplitude, and the length of the groundwater wave; flux is inversely proportional to tidal period. The duration of discharge flux exceeds the duration of recharge flux over one tidal period; and discharge flux continues for some time following low tide. Models compare favorably with laboratory observations and are applied to a South Atlantic Bight study area, where tide generates an 11-m3 groundwater tidal prism per m of shoreline, and drives 81 m3 s??1 to the study area, which describes 23% of an observational estimate. In a marine water body, the discharge component of any oscillatory benthic water flux is submarine groundwater discharge. Benthic flux transports constituents between groundwater and surface water, and is a process by which pollutant loading and saltwater intrusion may occur in coastal areas. 相似文献