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141.
Abstract

The study of sediment load is important for its implications to the environment and water resources engineering. Four models were considered in the study of suspended sediment concentration prediction: artificial neural networks (ANNs), neuro-fuzzy model (NF), conjunction of wavelet analysis and neuro-fuzzy (WNF) model, and the conventional sediment rating curve (SRC) method. Using data from a US Geological Survey gauging station, the suspended sediment concentration predicted by the WNF model was in satisfactory agreement with the measured data. Also the proposed WNF model generated reasonable predictions for the extreme values. The cumulative suspended sediment load estimated by this model was much higher than that predicted by the other models, and is close to the observed data. However, in the current modelling, the ANN, NF and SRC models underestimated sediment load. The WNF model was successful in reproducing the hysteresis phenomenon, but the SRC method was not able to model this behaviour. In general, the results showed that the NF model performed better than the ANN and SRC models.

Citation Mirbagheri, S. A., Nourani, V., Rajaee, T. & Alikhani, A. (2010) Neuro-fuzzy models employing wavelet analysis for suspended sediment concentration prediction in rivers. Hydrol. Sci. J. 55(7), 1175–1189.  相似文献   
142.
Excessive terrestrial nutrient loadings adversely impact coral reefs by primarily enhancing growth of macroalgae, potentially leading to a phase‐shift phenomenon. Hydrological processes and other spatial and temporal factors affecting nutrient discharge must be examined to be able to formulate effective measures for reducing nutrient export to adjacent reefs. During storm events and baseflow periods, water samples were obtained from the tropical Todoroki River, which drains an intensively agricultural watershed into Shiraho coral reef. In situ nutrient analyzers were deployed for 6 months to hourly measure dissolved nutrient (NO3‐N and PO43−‐P) concentrations. Total phosphorus (TP) and suspended solid concentration (TSS) were increased by higher rainfall intensity (r = 0·94, p < 0·01) and river discharge Q (r = 0·88, p < 0·01). In contrast, NO3‐N concentration tends to decrease drastically (e.g. from 3 to 1 mg l−1) during flood events. When base flow starts to dominate afterwards, NO3‐N manifested an increasing trend, but decreases when baseflow discharge becomes low. This counter‐clockwise hysteresis for NO3‐N highlights the significant influence of groundwater discharge. N delivery can therefore be considered a persistent process compared to sediment and P discharge, which are highly episodic in nature. Based on GIS analysis, nutrient concentration along the Todoroki River was largely affected by the percentage of sugarcane/bare areas and bedrock type. The spatial distribution of N concentration in the river reflects the considerable influence of subsurface geology—higher N levels in limestone‐dominated areas. P concentrations were directly related to the total length of artificial drainage, which enhances sediment transport. The use of high‐resolution monitoring data coupled with GIS‐based spatial analysis therefore enabled the clarification of control factors and the difference in the spatio‐temporal discharge characteristics between N and P. Thus, although erosion‐reduction schemes would reduce P discharge, other approaches (e.g. minimize fertilizer) are needed to reduce N discharge. Copyright © 2010 John Wiley & Sons, Ltd.  相似文献   
143.
鄂东北大别杂岩中混合岩形成的动力学机制   总被引:3,自引:1,他引:3  
王江海  杨问华 《地质学报》1994,68(4):308-323
本文针对中小位移量伸缩缝构造进行设计研究,提出了一种常温固化型桥梁伸缩缝。经过对伸缩量Δ20cm,Δ=40cm的多座桥梁的实验应用表明,这是一种适用于中小位移量桥梁中性能良好的伸缩缝,施工简便。其桥缝具体结构为,在两侧拍击区采用钢纤维混凝土增,缝内用高分子聚合物与一定比例的水泥及掺合物拌和均匀,经一段时间与桥面和加固铺装层固化成具有较高弹性和一定强度的整体式桥梁伸缩缝。其效果良好,供应用参考。  相似文献   
144.
将多元校正分析法应用于配位滴定中,以EDTA为滴定剂,玻璃电极为指示电极,饱和甘汞电极为参比电极。依据电位滴定原理,对混合三组分:Cu ̄(2+)、Cd ̄(2+)、Zn ̄(2+)、及Cu ̄(2+)、CO ̄(2+)、Ni ̄(2+)进行测定,各金属离子之间的△logK在0.04~2.34之间,计算误差一般小于土10%。  相似文献   
145.
High volume bulk aerosol samples were collected continuously at three Antarctic sites: Mawson (67.60° S, 62.50° E) from 20 February 1987 to 6 January 1992; Palmer Station (64.77° S, 64.06° W) from 3 April 1990 to 15 June 1991; and Marsh (62.18° S, 58.30° W) from 28 March 1990, to 1 May 1991. All samples were analyzed for Na+, SO 4 2– , NO 3 , methanesulfonate (MSA), NH 4 + ,210Pb, and7Be. At Mawson for which we have a multiple year data set, the annual mean concentration of each species sometimes vary significantly from one year to the next: Na+, 68–151 ng m–3; NO 3 , 25–30 ng m–3; nss SO 4 2– , 81–97 ng m–3; MSA, 19–28 ng m–3; NH 4 + , 16–21 ng m–3;210Pb, 0.75–0.86 fCi m–3. Results from multiple variable regression of non-sea-salt (nss) SO 4 2– with MSA and NO 3 as the independent variables indicates that, at Mawson, the nss SO 4 2– /MSA ratio resulting from the oxidation of dimethylsulfide (DMS) is 2.80±0.13, about 13% lower than our earlier estimate (3.22) that was based on 2.5 years of data. A similar analysis indicates that the ratio at Palmer is about 40% lower, 1.71±0.10, and more comparable to previous results over the southern oceans. These results when combined with previously published data suggest that the differences in the ratio may reflect a more rapid loss of MSA relative to nss SO 4 2– during transport over Antarctica from the oceanic source region. The mean210Pb concentrations at Palmer and Marsh and the mean NO 3 concentration at Palmer are about a factor of two lower than those at Mawson. The210Pb distributions are consistent with a210Pb minimum in the marine boundary layer in the region of 40°–60° S. These features and the similar seasonalities of NO 3 and210Pb at Mawson support the conclusion that the primary source regions for NO 3 are continental. In contrast, the mean concentrations of MSA, nss SO 4 2– , and NH 4 + at Palmer are all higher than those at Mawson: MSA by a factor of 2; nss SO 4 2– by 10%; and NH 4 + by more than 50%. However, the factor differences exhibit substantial seasonal variability; the largest differences generally occur during the austral summer when the concentrations of most of the species are highest. NH 4 + /(nss SO 4 2– +MSA) equivalent ratios indicate that NH3 neutralizes about 60% of the sulfur acids during December at both Mawson and Palmer, but only about 30% at Mawson during February and March.  相似文献   
146.
用非色散红外气体分析仪进行大气CO2本底浓度的测量   总被引:7,自引:1,他引:7  
按WMO关于开展全球CO2监测的要求,在对引进设备进行改进的情况下,建立了我国开展大气CO2本底浓度连续测量的红外气体分析测量系统及有关方法。系统的测量精度优于0.1ppm,完全满足全球本底测量的要求,并具有较好的国际可比性。在此基础上,首次取得了我国大陆上空大气CO2的本底浓度资料。  相似文献   
147.
148.
含氡地下水对某些地方病的防治作用   总被引:1,自引:0,他引:1  
杨福山 《铀矿地质》1991,7(4):218-222
  相似文献   
149.
高岭石的结晶有序度及其对纸张涂布粘浓度的影响   总被引:5,自引:0,他引:5  
周国平  林毓川 《矿物学报》1991,11(3):267-273
粘浓度是纸张涂布的一项重要指标,测定的变化范围从46.4—72%。用Hinckley方法测定了高岭石的结晶度指数,从0.57变化至1.40。当粘浓度>67%时,结晶度指数>1。粘浓度<67%,结晶度指数<1,有序高岭石有利于粘浓度提高。随着结构无序化,晶粒变小,晶片变薄,比表面增加,晶体边缘和角易破损,使粘浓度降低。结构无序化破坏了颗粒的均匀性,使颗粒长/厚比增加,粘浓度降低。高岭石八面体中Fe~(3+)的存在一定程度上影响了有序度。  相似文献   
150.
气象因子对近地面臭氧污染影响的研究   总被引:15,自引:0,他引:15  
徐家骝  朱毓秀 《大气科学》1994,18(6):751-757
本文通过对1993年春季和春夏之交的O3浓度逐日变化、日变化和气象因子关系的分析,提出了影响O3浓度的主导气象因子和不同情况下形成高浓度O3的主要因子,提出了大风速对逐日变化中O3浓度特高及浓度日变化峰值的重要作用,并指出高温、低湿、小风并不是在所有情况都是促成高浓度O3的因子。另外,雾也可以成为近地面O3浓度增值的因素,主要原因是雾内湍流发展将高浓度O3大量输向下方。  相似文献   
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