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261.
单环刺螠纤溶酶的分离纯化及其性质的初步研究 总被引:3,自引:1,他引:2
从单环刺中制得单一组分的纤溶活性纤溶酶,并对其性质进行初步研究.单环刺体组织液经离心,超滤,离子交换层析,凝胶过滤等方法进行分离纯化,制得单一洗脱峰酶组分,经Native-PAGE电泳分析,SDS-PAGE电泳分析和飞行质谱分析,鉴定了酶制品纯度和相对分子量,进行了体外溶血栓试验.所得纯品UFEIa水解酪蛋白的比活力为442.0 U/mg,纯化倍数为12.1倍,回收率为27.0%.UFEIa为单一组分,相对分子量约23 800 Da.体外溶血栓实验表明此纤溶活性蛋白酶与蚓激酶相比具有很好的溶血栓活性. 相似文献
262.
一种新的L-集表现定理 总被引:1,自引:1,他引:0
在隶属度值格仅为完备格的条件下,研究了L-集轮和L-开集轮的特征性质,并以2种集轮为工具给出基于L-集轮和L-开集轮的L-集表现定理.由于隶属度值格仅为完备格,得到的L-集表现定理更有一般意义. 相似文献
263.
平行结构建筑是3维城市中建筑的主体,随着建筑风格的多元化,非平行结构建筑所占的比重越来越大,因此必须对其多尺度表达的方法进行研究.此处根据复杂程度的不同将建筑分为简单建筑和特殊建筑两类.在简单建筑的化筒中,首先讨论了倾斜房顶的几何表示方法,在此基础上建立了房顶的关系信息,采用成组处理与斜面的扯直拉平算法相结合的方式实现了简单建筑的化简.在分析复杂建筑倾斜面结构特点的基础上设计了适于复杂建筑的化简方法,并针对两类典型建筑进行了实验. 相似文献
264.
265.
The response of the eastern tropical Indian Ocean(ETIO) to heat fluxes of equal amplitude but opposite sign is investigated using the Community Earth System Model(CESM). A significant positive asymmetry in sea surface temperature(SST) is found over the ETIO—the warming responses to the positive forcing exceeds the cooling to the negative forcing. A mixed layer heat budget analysis is carried out to identify the mechanisms responsible for the SST asymmetry. Results show that it is mainly ascribed to the ocean dynamical processes, including vertical advections and diffusion. The net surface heat flux, on the contrary, works to reduce the asymmetry through its shortwave radiation and latent heat flux components. The former is due to the nonlinear relationship between SST and cloud, while the latter is resulted mainly from Newtonian damping and air-sea stability effects. Changes in the SST skewness are also evaluated, with more enhanced negative SST skewness over the ETIO found for the cooling than heating scenarios due to the asymmetric thermocline-SST feedback. 相似文献
266.
The northeastern shelf margin of the South China Sea(SCS) is characterized by the development of large scale foresets complexes since Quaternary. Based on integral analysis of the seismic, well logging and paleontological data, successions since ~3.0 Ma can be defined as one composite sequence, consist of a set of regional transgressive to regressive sequences. They can be further divided into six 3 rd order sequences(SQ0–SQ5) based on the Exxon sequence stratigraphic model. Since ~1.6 Ma, five sets of deltaic systems characterized by development of wedge-shaped foresets complexes or clinoforms had been identified. High-resolution seismic data and the thick foresets allowed further divided of sub-depositional sequences(4 th order) of regression to transgression, which is basically consistent with published stacked benthic foram O-isotope records. Depositional systems identified in the study area include deltaic deposits(inner-shelf deltas and shelf-edge deltas), incised valleys, and slope slumping massive deposits. Since ~1.6 Ma, clinoforms prograded from the southern Panyu Lower Uplift toward the northern Baiyun Depression, shelf slope break migrated seaward, whereas the shelf edge of SQ0 migrated landward. The development of incised valleys in the continental shelf increased upward,especially intensive on the SB3 and SB2. The slumping massive deposits increased abruptly since SB2, which corresponds to the development of incised valleys. The evolution of depositional systems of continental slope mainly controlled by the combined influence of sea level changes, tectonic movements, sediment supply and climate changes. Since ~3.0 Ma, relative sea level of the northern SCS had been experienced transgression(~3.0 Ma BP) to regression(~1.6 Ma BP). The regional regression and maximum transgressions of the composite sequences were apparently enhanced by uplift or subsidence related to tectono-thermal events. In addition,climatic variations including monsoon intensification and the mid-Pleistocene transition may have enhanced sediment supply by increasing erosion rate and have an indispensable influence on the development of the incised valleys and 5 sets of deltaic systems since ~1.6 Ma. 相似文献
267.
西南印度洋中脊表层沉积物非碳酸盐组分的粒度特征及其地质意义 总被引:1,自引:0,他引:1
The carbonate-free fraction of 20 surface sediments collected from the ultraslow-spreading Southwest Indian Ridge(SWIR) was studied by grain size analysis and mineralogical analysis with X-ray powder diffraction(XRD),stereo microscopy and scanning electron microscopy(SEM). The characteristics of the carbonate-free fraction of the sediments were obtained, and related influential factors were discussed. The results show that the mean grain size of this fraction is in 1.96Φ–8.19Φ, with poorly sorting and unimodal, bimodal or irregular bimodal distribution patterns. Four grain size end members of the fraction are derived with the End Member Model method. The finest end member EM1 shows a significant contribution of terrigenous materials of the aeolian input and sediment carried by the bottom current. End member EM2 with medium size mainly reflects sediment of a siliceous bioclast origin. EM3 and EM4 are interpreted as representing the coarser volcanic materials related to bedrock weathering or volcanic activities. Multi-provenance is the dominant factor controlling the grain size pattern of the carbonate-free fraction of the sediments in that area. In addition, sediment transport processes such as the bottom current and wind are the minor factors that influence the grain size distribution of the carbonate-free fraction sediments. 相似文献
268.
269.
航空重力梯度测量属于被动探测,抗干扰能力强,如果能和其他探潜手段相配合将极大地提高航空搜潜的效率。针对航空重力梯度测量是否能够用于探测潜艇的问题,依据俄亥俄级弹道导弹核潜艇的结构特点,建立了适用于重力梯度计算的潜艇模型,分别给出了潜艇外壳、内部质量亏损产生的重力垂直梯度的计算方法,并对不同精度重力梯度仪可探测的潜艇重力垂直梯度值进行了计算,从航空反潜的角度对探测潜艇效果进行了分析。经计算表明,如航空重力梯度仪精度达到10~(-2) E,将具备一定的实际探潜效能;如精度达到10~(-4) E,反潜机搜索宽度可与现有航空磁性探潜相当。 相似文献
270.