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51.
三江平原位于我国东北的边陲,系黑龙江、松花江、乌苏里江汇流而成的冲积平原。其位置在东经129°11′20″至135°5′10″,北纬43°49′55′至48°27′40″(图1)。  相似文献   
52.
1 Introduction Actinisanimportantcontractileproteinineukary oticcells .Itisoneofthetwomajorcomponentsin volvedinthecontractionofmusclecells .Innon mus clecells ,itisthemajorpartofcytoskeletoninvolvedinmanyprocessessuchascellmotility ,endocytosis ,exocyt…  相似文献   
53.
黄河流域近40年日照百分率的气候变化特征   总被引:34,自引:1,他引:34  
买苗  曾燕  邱新法  高苹  王萧宇 《气象》2006,32(5):62-66
利用黄河流域及其周边146个气象站1960--2000年逐月日照百分率资料,研究分析了黄河流域日照百分率的气候变化趋势。结果表明,就整个流域平均而言,日照百分率呈明显下降趋势,黄河流域年平均日照百分率在20世纪90年代较60年代下降了2.49%;日照百分率的下降主要表现在夏季和冬季,春季和秋季下降不明显。对日照百分率气候变化的空间分析表明,除极少数台站的日照百分率呈略有上升趋势外(主要出现在流域上游),黄河流域日照百分率的下降表现得非常明显,遍布整个流域的中、下游。  相似文献   
54.
肇庆市一次超级单体的多普勒雷达资料分析   总被引:5,自引:1,他引:5  
郭媚媚  麦冠华  胡胜  何华庆 《气象》2006,32(6):97-101
利用广州S波段多普勒雷达资料,对2004年7月1日夜间发生在广东省肇庆市的一次强对流天气过程进行分析,发现引起这次强对流的风暴具有超级单体风暴的特征。这个超级单体南边出现两条明显的出流边界,分别位于钩状回波的西南和东南。相应的中低层径向速度图呈现一个弱中尺度气旋,旋转速度达12m·s-1。该超级单体的移动方向在盛行风向的右侧约30°,属于右移风暴。  相似文献   
55.
主要介绍新疆维吾尔自治区地震局放射性同位素碳测年实验室的14C测年原理,样品的前处理、样品的化学制备,低水平放射性测量方法及测定年代。首次公布一批14C年代测定数据。  相似文献   
56.
The Seve Nappes consist of long-transported thrust sheets belonging to the Upper Allochthon within the Scandinavian Caledonides. Eclogites from two different megalenses within the Seve Nappe Complex in Norrbotten (northern Sweden) have been dated with the Sm-Nd method. The two eclogite-bearing megalenses have been subjected to different pressure and temperature conditions during the high-pressure metamorphism. Garnet + omphacite + whole-rock from TS2 within the Tsäkkok Lens give an age of 505±18 Ma (2), I=0.512231±0.000024, MSWD=0.10. Garnet and whole-rock from TS5 and whole-rock TS3 also fall on the above isochron. The composite isochron gives an age of 503±18 Ma (2). These results are interpreted to date the peak of the high-pressure metamorphism (500–630° C and 12–15 kbars) for the Tsäkkok Lens. The eclogites in the Vaimok Lens (at Grapesvarre) were subjected to higher pressure and temperature conditions and more extensive reequilibration during the early cooling stages. Retrograde breakdown-reactions accompanied by retrograde zoning of relict garnet seems to be associated with disturbance of the Sm-Nd isotopic systems. In contrast, a sample with unzoned garnet and well preserved high-pressure mineralogy from Grapesvarre gives a Sm-Nd garnet + omphacite age of 503±14 Ma (2), I = 0.512010±0.000038 (2). The ages for the Seve eclogites are significantly older than the Sm-Nd eclogite dates from the Western Gneiss Region of Norway (WGR), suggesting the existence of at least two eclogite-forming events in the Caledonide Orogen. The younger event has been related to the main continent-continent collision stage of the Caledonian Orogeny, while the older event that led to the production of the Norrbotten eclogites must have taken place several hundred kilometres to the north and in a different tectonic setting more oceanward to the WGR. It appears that the older event (ca. 505 Ma) was restricted to the subduction of dyke-intruded sedimentary cover rocks which are thought to represent the rifted edge of the Baltic continent.  相似文献   
57.
一种准确而快速的运动目标检测算法   总被引:2,自引:0,他引:2  
运动目标的检测是计算机视觉和图像编码研究的主要内容,有着广泛的应用领域.减背景法是常用的方法之一,但其受环境光照影响;而帧差法又不能完全提取出目标的所有相关点.针对传统运动目标检测算法的不足,提出基于动态阈值的减背景法与帧差法相结合的运动目标检测算法.实验证明,算法既能完全提取出目标的所有相关点,又适应复杂变化的环境,运动目标检测的精确度和速度都有了明显的提高.  相似文献   
58.
The mobilization of arsenic (As) to the groundwater was studied in a shallow Holocene aquifer on the Red River flood plain near Hanoi, Vietnam. The groundwater chemistry was investigated in a transect of 100 piezometers. Results show an anoxic aquifer featuring organic carbon decomposition with redox zonation dominated by the reduction of Fe-oxides and methanogenesis. Enhanced PCO2 pressure causes carbonate dissolution to take place but mainly in the soil and unsaturated zone. The concentration of As increases over depth to a concentration of up to 550 μg/L. Most As is present as As(III) but some As(V) is always found. Arsenic correlates well with NH4, relating its release to organic matter decomposition and the source of As appears to be the Fe-oxides being reduced. Part of the produced Fe(II) is apparently reprecipitated as siderite containing less As. Results from sediment extraction indicate most As to be related to the Fe-oxide fractions. The measured amount of sorbed As is low. In agreement, speciation calculations for a Fe-oxide surface suggest As(III) to constitute only 3% of the surface sites while the remainder is occupied by carbonate and silica species. The evolution in water chemistry over depth is homogeneous and a reactive transport model was constructed to quantify the geochemical processes along the vertical groundwater flow component. A redox zonation model was constructed using the partial equilibrium approach with organic carbon degradation in the sediment as the only rate controlling parameter. Apart from the upper meter a constant degradation rate of 0.15 C mmol/L/yr could explain the redox zonation throughout the aquifer. Modeling also indicates that the Fe-oxide being reduced is of a stable type like goethite or hematite. Arsenic is contained in the Fe-oxides and is first released during their dissolution. Our model further suggests that part of the released As is adsorbed on the surface of the remaining Fe-oxides and in this way may be retarded.  相似文献   
59.
60.
A short‐term flood inundation prediction model has been formulated based on the combination of the super‐tank model, forced with downscaled rainfall from a global numerical weather prediction model, and a one‐dimensional (1D) hydraulic model. Different statistical methods for downscaled rainfall have been explored, taking into account the availability of historical data. It has been found that the full implementation of a statistical downscaling model considering physically‐based corrections to the numerical weather prediction model output for rainfall prediction performs better compared with an altitudinal correction method. The integration of the super‐tank model into the 1D hydraulic model demonstrates a minimal requirement for the calibration of rainfall–runoff and flood propagation models. Updating the model with antecedent rainfall and regular forecast renewal has enhanced the model's capabilities as a result of the data assimilation processes of the runoff and numerical weather prediction models. The results show that the predicted water levels demonstrate acceptable agreement with those measured by stream gauges and comparable to those reproduced using the actual rainfall. Moreover, the predicted flood inundation depth and extent exhibit reasonably similar tendencies to those observed in the field. However, large uncertainties are observed in the prediction results in lower, flat portions of the river basin where the hydraulic conditions are not properly analysed by the 1D flood propagation model. Copyright © 2013 John Wiley & Sons, Ltd.  相似文献   
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