水文模型参数多目标率定及最优非劣解优选     

周建中  卢韦伟  孙娜  叶磊  张海荣  陈璐 《水文》2017,37(2):1-7

针对概念性水文模型参数众多、相互制约,且多目标参数优化率定最优参数求解困难、易受决策者主观因素影响的问题,采用多目标优化算法对水文模型参数进行率定,得到模型参数最优非劣解集,在此基础上,引入最小最大后悔值决策理论,并结合Pareto支配基本理论,提出了一种多目标最优非劣解选取准则。以柘溪流域为研究对象,采用三目标MOSCDE优化率定新安江模型的参数,并与单目标SCE-UA优化结果进行对比分析。结果表明,提出的非劣解选取方法可以有效从大规模非劣解集中筛选出最优非劣解,大大缩短参数率定耗时。  相似文献   

CBERS02B 卫星CCD 相机在轨辐射定标\n与真实性检验     

巩慧 《遥感学报》2010,14(1):7-22

利用贡格尔实验场对CBERS02B卫星进行场地反射率基法辐射定标, 获得CCD相机可见近红外波段的绝对辐射定标系数, 利用敦煌实验场对定标系数进行了真实性检验。结果表明: 此次定标结果和测量值非常吻合, 定标系数可信度高。  相似文献   

基于岭估计的相机标定方法     

于英  陈继华 《测绘科学》2010,35(3):80-81,76

相机内外参数标定是摄影测量的一个关键问题,相机参数的选取又是决定相机标定质量的重要因素,且不同等级的相机其参数的选择往往很难确定,常导致所选取的参数之间存在相关性,影响相机标定质量。相机参数间的相关性一般可以通过验后未知数之间的相关系数矩阵发现,提出了基于岭估计的相机标定方法,利用本方法可以提高参数求解精度。  相似文献   

航空摄影测量数码相机的检校方法研究     

李绍刚  陶安利  杨铁利  吴晓明 《测绘科学》2010,35(6):50-51,61

通过分析航空摄影中数码相机的误差来源及规律,提出了利用专用检校场检校数码相机的数学模型、理论方法和实用检校步骤,并在分析实际检测数据的基础上,完善了控制点的获取效率进而改进了控制点的布设方案,最后通过实验论证了此方法的高精度性、可靠性与可行性。  相似文献   

大于40mm颗粒含量对回填土压实系数的影响及校正度研究     

李冰洁  万广利  刘长吉 《世界地质》2014,33(1):240-245

依托浙北1 000 kV变电站新建工程,对28个基槽回填土试样的压实系数试验结果进行研究。试验所用指标主要为干密度、最大干密度、40 mm颗粒含量等,基于主成分分析法的基本原理,找出对该工程回填土试样试验结果产生较大影响的因素。结果表明,40 mm颗粒含量对于压实系数的准确测定存在影响,而在普通压实系数测定过程中往往忽略这一因素,因此,有必要根据40 mm颗粒含量对试样的压实系数进行校正。通过引入校正度这一概念,反映出随着40 mm颗粒含量的增加,实测结果对理论曲线的离散度增大,试验结果的精度逐渐降低。  相似文献   

The relationship between hydrocarbon accumulation and Mississippi Valley‐type Pb‐Zn mineralization of the Mayuan metallogenic belt,the northern Yangtze block,SW China: Evidence from ore geology and Rb‐Sr isotopic dating     

Guozhi Wang  Zhu Huang  Fufeng Zhao  Na Li  Yuzhen Fu 《Resource Geology》2020,70(2):188-203

The coexistence of Pb‐Zn deposits and oil/gas reservoirs demonstrates that a close genetic connection exists between them. The spatiotemporal relationship between Pb‐Zn mineralization and hydrocarbon accumulation is the key to understanding this genetic connection. The Mayuan large‐scale Pb‐Zn metallogenic belt is composed of a number of Mississippi Valley‐type (MVT) Pb‐Zn deposits that were recently discovered on the northern margin of the Yangtze Block, China. It is hosted in the dolostone of the Sinian (Ediacaran) Dengying Formation (Z₂dn). In addition to the abundant bitumen in the Mayuan Pb‐Zn metallogenic belt, the paleo‐oil reservoir and the MVT Pb‐Zn deposit overlap in space. In this study, two precise ages of 468.3 ± 3.8 Ma and 206.0 ± 6.5 Ma were obtained via the Rb‐Sr isotopic dating of galena and sphalerite from the Mayuan Pb‐Zn metallogenic belt, respectively. The early metallogenic age of 468.3 ± 3.8 Ma is similar to the previously published age of 486 ± 12 Ma. The age of 206.0 ± 6.5 Ma is consistent with the age of the metallogenic event that occurred at 200 Ma in the Upper Yangtze Pb–Zn metallogenic province of the Sichuan‐Yunnan‐Guizhou polymetallic zone, which is located on the southwest margin of the Sichuan Basin, suggesting that the metallogenic effects of this period were regional in scale in the peripheral areas of the Sichuan Basin. Previous studies have shown that two periods of hydrocarbon accumulation occurred in the oil/gas reservoir that coexists with the Pb‐Zn deposits in the study area. The Pb‐Zn mineralization at 468.3 ± 3.8 Ma occurred during the first period of hydrocarbon accumulation, while the second mineralization at 206.0 ± 6.5 Ma occurred during the transformation of the paleo‐oil reservoir to a paleogas reservoir. The spatial relationship between the paleo‐oil/‐gas reservoir and the MVT Pb‐Zn deposits and the temporal relationship between mineralization and hydrocarbon accumulation show that a close genetic relationship exists between the MVT Pb‐Zn mineralization and hydrocarbon accumulation. Analysis of metals in the source rocks forming the paleo‐oil/‐gas reservoirs show that source rocks which formed paleo‐oil/‐gas reservoirs may have provided metals for Pb‐Zn mineralization. Both the paleo‐oil/‐gas reservoirs and Pb‐Zn mineralizing fluids had the same origin.  相似文献   

TOPMODEL: A critique     

KEITH BEVEN 《水文研究》1997,11(9):1069-1085

TOPMODEL (a TOPography based hydrological MODEL) is now 20 years old and has been the subject of numerous applications to a wide variety of catchments. This paper represents a critical review of some of the issues involved in application of the TOPMODEL concepts, including the basic assumptions involved; the derivation of topographic index distributions from digital terrain data; additional model components; meaning and calibration of the model parameters; and issues involved in model validation and predictive uncertainty. The aim is to provoke a thoughtful approach to hydrological modelling and the interaction of modelling and field work. Some recommendations are made for future modelling practice. © 1997 John Wiley & Sons, Ltd.  相似文献   

Data assimilation in groundwater modelling: ensemble Kalman filter versus ensemble smoothers          下载免费PDF全文

Liangping Li  Ryan Puzel  Arden Davis 《水文研究》2018,32(13):2020-2029

Groundwater modelling calls for an effective and robust data integrating method to fill the gap between the model and observation data. The ensemble Kalman filter (EnKF), a real‐time data assimilation method, has been increasingly applied in multiple disciplines such as petroleum engineering and hydrogeology. In this approach, a groundwater model is updated sequentially with measured data such as hydraulic head and concentration. As an alternative to the EnKF, the ensemble smoother (ES) has been proposed for updating groundwater models using all the data together, with much less computational cost. To further improve the performance of the ES, an iterative ES has been proposed for continuously updating the model by assimilating measurements together. In this work, we compare the performance of the EnKF, the ES, and the iterative ES using a synthetic example in groundwater modelling. Hydraulic head data modelled on the basis of the reference conductivity field are used to inversely estimate conductivities at unsampled locations. Results are evaluated in terms of the characterization of conductivity and groundwater flow predictions. It is concluded that (a) the iterative ES works better than the standard ES because of its continuous updating and (b) the iterative ES could achieve results comparable with those of the EnKF, with less computational cost. These findings show that the iterative ES should be paid much more attention for data assimilation in groundwater modelling.  相似文献   

Landsat-8 OLI卫星数据的大气校正检验及其应用     

阿如汗  青松  包玉海 《海洋科学》2018,42(6):107-115

本文检验了Vanhellemont和Ruddick算法在浑浊的海洋沿岸水体中的适用性。采用基于Vanhellemont和Ruddick算法对2013—2015年黄河口水体的landsat-8 OLI数据进行大气校正,该算法得到的OLI反射率与黄河口高光谱实测反射率较一致, R为0.95,在483 nm(蓝)、561 nm(绿)、655 nm(红)波段处平均相对误差为16.4%、17.3%和25.7%。MODIS和Landsat-8 OLI数据获取的悬浮物浓度之间一致性较好, R为0.85,平均相对误差为20.5%,表明该算法适用于黄河口水体。基于时间序列OLI数据,得到了悬浮物浓度时空分布特征。黄河口悬浮物浓度变化差异主要由风速和输沙量引起的,风速和输沙量对悬浮物浓度的影响存在一定的时间滞后现象。  相似文献   

Eutrophication In Lake Rotorua. 2. Using ROTAN and OVERSEER to model historic,present and future nitrogen loads     

J. Christopher Rutherford  Christopher C. Palliser  Alastair MacCormick 《新西兰海洋与淡水研究杂志》2019,53(1):128-161

OVERSEER is used in New Zealand to estimate nutrient losses from farmland, but does not quantify subsequent movement through the catchment, or attenuation. This paper uses the ROTAN model, based on the Scandinavian HBV-N model, to route nitrogen losses from 1900–2015 to Lake Rotorua where groundwater age ranges from 14 to 170 years. ROTAN conceptualises three delivery pathways (quickflow, groundwater and streamflow) with different attenuation. When calibrated to measured stream and groundwater concentrations, several combinations of attenuation gave equally good fits largely because of sparse and uncertain input and calibration data. Nevertheless, lake N loads were predicted for current land use (754?±?39?t y^?1) and with proposed N loss reductions (431?±?26?t y^?1). Probabilities were also calculated that the reductions are more (12%–18%) or less (82%–88%) than required to meet the target lake N load (405?t y^?1). ROTAN shows promise for calculating nitrogen movement in catchments dominated by groundwater where there is limited data.  相似文献