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31.
rmIoxThe averag annual dischaIge of the Zhujiang Xiver is 3. 32 x l0ll m3, which ranks theZhujiang River just end to the Changjiang River in China. The dischnye occutring duringthe fltal m between APril and ffepteTnber accounts for 80% of the yearly total. The Zhu-jiang hiver has a yeaIy sediment load of about 1 x l08 tons, which also concentrates in theM arn (Zhao, l990; Chen et al., 1998). The Zhujiang Xiver delta,which has l2 cities ofdifferent sizes and more than 40 towns with a po… 相似文献
32.
33.
低分子肝素作为一种抗血栓的多糖药物在临床中已应用了二十多年 ,目前已作为外科预防血栓形成药物 ,并在治疗急性静脉栓塞紊乱方面取代了未分级肝素。因肝素的来源和制备的方法不同使低分子肝素的精细结构不同 ,低分子肝素结构的复杂性 ,使得各产品的生物活性 ,例如抗蛋白酶活性不同 ,从而导致其临床使用的标准不同。该文将对低分子肝素的制备方法及其结构和抗蛋白酶活性的差异进行报导 相似文献
34.
研究肝素酶Ⅰ(来源于Flavobacterumheparinase,EC4.2.2.7)对人工合成的且含有与抗凝血酶Ⅲ特定结合位点的肝素五糖(SHP)的酶解作用,并对酶解作用的动力学进行研究。利用强阴离子高效液相色谱(SAX-HPLC)对酶解混合物进行分离,利用质谱(ESIMS)和核磁共振波谱(1H-NMR)技术对得到的二糖和三糖的结构进行确证。研究结果表明,这种被作为肝素反向试剂的肝素酶Ⅰ可水解人工所合成的肝素五糖,从而使之丧失抗Xa因子活性。 相似文献
35.
自北赤道流延伸而来的黑潮,起源于我国台湾省的东南海域。当黑潮沿着台湾岛东岸北上时,它的主轴通过苏澳-与那国岛断面,自北太平洋进入我国东海,成为我国东、黄海海流系统的“大动脉”。显然,黑潮的流速结构及其变化,对东、黄海水文特征的分布、变化以及我国东部沿海地区的气候,特别是旱涝现象,都有着密切的关系。所以,有关这一问题的探讨是很有意义的。而欲研究黑潮的上述问题,取苏澳-与那国岛断面作为探讨的核心是很合适的,因为这个断面不仅离黑潮源地较近,而且位于黑潮进入东海首当其冲的关键性区域。
关于黑潮在这一断面上海洋水文状态的变化情况,日本学者须田晥次(K.Suda,1937-1938)曾作过广泛的研究,他主要分析了黑潮源地区域标量场(温、盐、密度等)的逐月变化特征。本文拟引用须田当年所列举的温、盐度资料,来研究黑潮的流速结构(主要是流速分布和输送量)及其季节变化,并结合现有的海面风应力资料,试图对黑潮输送量的季节变化及其原因作一初步的探讨,并作为进一步研究黑潮变动规律的参考。 相似文献
36.
藻类功能食品的物质基础与研究开发现状 总被引:3,自引:0,他引:3
对藻类功能食品的研究和开发现状作综述报道。涉及的主要内容有:作为功能食品物质基础的食物纤维、PUFA、维生素、矿物质和微量元素、氨基酸以及其它有生理活性的物质。 相似文献
37.
Aproposeddirectionalfunctionandwind-wavedirectionalspectrum¥WenShengchang;WuKejian;GuanChanglong;SunShicaiandZhangDacuo(Recei... 相似文献
38.
Moo Hee Kang Hyun-Chul Han Hyesu Yun Gee Soo Kong Kyong O. Kim Youn Soo Lee 《Marine Geophysical Researches》2007,28(3):257-269
A seamount chain with an approximately WNW trend is observed in the northeastern Ulleung Basin. It has been argued that these
seamounts, including two islands called Ulleung and Dok islands, were formed by a hotspot process or by ridge related volcanism.
Many geological and geophysical studies have been done for all the seamounts and islands in the chain except Anyongbok Seamount,
which is close to the proposed spreading ridge. We first report morphological characteristics, sediment distribution patterns,
and the crustal thickness of Anyongbok Seamount using multibeam bathymetry data, seismic reflection profiles, and 3D gravity
modeling. The morphology of Anyongbok Seamount shows a cone shaped feature and is characterized by the development of many
flank cones and flank rift zones. The estimated surface volume is about 60 km3, and implies that the seamount is smaller than the other seamounts in the chain. No sediments have been observed on the seamount
except the lower slope, which is covered by more than 1,000 m of strata. The crustal structure obtained from a 3D gravity
modeling (GFR = 3.11, SD 3.82 = mGal) suggests that the seamount was formed around the boundary of the Ulleung Plateau and
the Ulleung Basin, and the estimated crustal thickness is about 20 km, which is a little thicker than other nearby seamounts
distributed along the northeastern boundary of the Ulleung Basin. This significant crustal thickness also implies that Anyongbok
Seamount might not be related to ridge volcanism. 相似文献
39.
-The hydrodynamic forces on a smooth inclined circular cylinder exposed to oscillating flow were experimentally investigated at Reynolds number (Re) in the range 40000-200000 and Keulegan-Capenter number (KC) in the interval from 5-40. In the test, Re number and KC number were varied systematically. The inertia force coefficient (Cu) and the drag force coefficient (CD) in Morison equation were determined from the measured loads and the water particle kinematics. In this analysis a modified form of Morison equation was used since it uses the normal velocity and acceleration. Thus, the applicability of the Cross Flow Principle was assumed. This principle, simply stated, is as follows: the force acting in the direction normal to the axis of a cylinder placed at some oblique angle with the direction of flow is expressed in terms of the normal component of flow only, and the axial component is disregarded. Both the total in-line force coefficient (CF) and transverse force (lift) coefficient (Cf) were analyzed 相似文献
40.
K. S. Jeong J. K. Kang K. Y. Lee H. S. Jung S. B. Chi S. J. Ahn 《Geo-Marine Letters》1996,16(2):123-131
In the northwestern margin of the Clarion and Clipperton fracture zones, manganese nodules are latitudinally variable in character, resulting from the progressive (re)generation of nodules since the Oligocene as the Pacific Plate migrates northwestward beneath the equatorial production zone. Complemented by the surface water productivity, bottom current activities have concentrated nodules in the Oligocene to Miocene siliceous clay. Resedimentation processes on nodules form three types of nodules with concentric structures and 10 Å-manganaterich bottoms, by periodically causing the diagenetic growth of nodules within the topmost sediment layer. 相似文献