Temperature‐ and size‐associated differences in the skeletal structures and osculum cross‐sectional area influence the pumping rate of contractile sponge Cinachyrella cf. cavernosa

Sponges alter the proportion of structural and morphological components such as spicule skeleton and number of oscula in response to environment, development and growth. Such mechanisms indicate morphological and physiological variations within populations. We measured the pumping rate of different sized specimens of contractile sponge Cinachyrella cf. cavernosa present in the intertidal rock pools, during morning and afternoon low tides along the central west coast of India. Additionally, we measured the exhalant opening (oscular cross‐sectional area—OSA), tissue density, spicule skeleton weight and the abundance of choanocyte chambers to assess the morphological variations. Water temperature and sponge size showed a significant positive effect on pumping rate. OSA and the number of oscula increased with sponge size, but the sponge volume‐specific pumping rate did not increase (0.029 ± 0.020 ml/s ml^‐1). Histological sections showed the abundance of chaonocyte chambers increased marginally with the sponge size, but the contraction state affected the count. Both tissue density and spicule skeleton weight were positively correlated with sponge size, particularly the increase in the size and number of spicule bundles radiating from the centre indicated a denser core in larger specimens. The subcortical lacunae and the peripheral choanosome with high abundance of canals appear to be the major volume reduction zones during contraction events. Our results indicate that the size and number of spicule bundles increase with sponge volume and the variation in temperature, contraction state, and size and number of oscula influence the pumping rate of C. cf. cavernosa.     

DISADOPTION OF MILK COWS BY FARMERS IN ILLINOIS: 1930–1978*

I am concerned with the opposite of diffusion, i.e., the patterns and processes that describe the contraction or disappearance of phenomena. Using change over time in the proportion of farms that do not have milk cows as a medium of investigation, I present evidence that the logistic curve provides a good temporal, non-spatial model of the data and that a periphery-to-core contraction model is significant in describing the spatial pattern.     

Petrogenesis and evolution of late Mesozoic granitic magmatism in the Hohhot metamorphic core complex,Daqing Shan,North China

Late Mesozoic granitoid plutons of four distinct ages intrude the lower plate of the Hohhot metamorphic core complex along the northern margin of the North China craton. The plutons belong to two main groups: (1) Group I, deformed granitoids (148 and 140 Ma subgroups) with high Sr, LREE, and Na₂O, low Y and Yb contents, high Sr/Y and La/Yb ratios, weak or no Eu anomalies, low Rb/Ba ratios, similar initial ⁸⁷Sr/⁸⁶Sr values (0.7064–0.7071) and low Mg^# (<37 mostly, 100?×?molar MgO/MgO + FeO _t ); (2) Group II, non-deformed granitoids (132 and 114 Ma subgroups) with low Sr, relatively low Na₂O, high Y and Yb contents, pronounced negative Eu anomalies, high Rb/Ba ratios, and initial ⁸⁷Sr/⁸⁶Sr values (0.7098–0.7161). The two groups share geochemical similarities in ?_Nd(t) (–11.3 to –15.4) and T _DM2 ages (1.85–2.18 thousand million years) as well as Hf isotopic ratios in zircons. Geochemical modelling (using the MELTS code) suggests that similar sources but different depths of magma generation produced the early, high-pressure low-Mg adakitic granitoids and late, low-pressure granitoids with A-type characteristics. The early granitoids likely represent a partially melted, deep-seated, thickened lower continental crust that involved a minor contribution from young materials, whereas the later group partially melted at shallower depths. This granitic magmatic evolution coincided with the tectonic transition from crustal contraction to extension.     

φ积分型压缩条件下弱相容映象的几个公共不动点定理

为了强化理论知识的应用,在这篇论文中,利用度量空间中自映象的弱相容性条件,讨论φ积分型压缩条件的公共不动点存在性和唯一性问题,证明了几个新的公共不动点定理,文章改进和发展了Pathk,Verma和张勇等的结果。     

滨州黄河公路大桥承台大体积混凝土防裂技术探讨

介绍了滨州黄河公路大桥承台大体积混凝土防止温度裂缝的主要措施和过程,并对其效果进行简要评析。从大体积混凝土的性质和特点出发进行探讨和研究,以使所采取的措施行之有效和切合实际。     

Parallel computation of seismic analysis of high arch dam

Parallel computation programs are developed for three-dimensional meso-mechanics analysis of fully-graded dam concrete and seismic response analysis of high arch dams （ADs）, based on the Parallel Finite Element Program Generator （PFEPG）. The computational algorithms of the numerical simulation of the meso-structure of concrete specimens were studied. Taking into account damage evolution, static preload, strain rate effect, and the heterogeneity of the meso-structure of dam concrete, the fracture processes of damage evolution and configuration of the cracks can be directly simulated. In the seismic response analysis of ADs, all the following factors are involved, such as the nonlinear contact due to the opening and slipping of the contraction joints, energy dispersion of the far-field foundation, dynamic interactions of the dam-foundation- reservoir system, and the combining effects of seismic action with all static loads. The correctness, reliability and efficiency of the two parallel computational programs are verified with practical illustrations.     

Folding of the Gediz Graben Fill,SW Turkey: Extensional and/or Contractional Origin?

Folds constitute a significant part within the dominantly extension-related deformation pattern of the Gediz Graben and their origin either extensional or contractional has been the subject of debate. Field and subsurface data presented in this paper suggest that folds of contractional and extensional origin coexist in the graben-fill sediments. Contractional folds are predominantly observed within the Alasehir formation. A north vergent, plunging, asymmetrical to overturned geometry characterizes these folds and they are commonly observed in association with south dipping both thrust and reverse faults; the presence of thrust/reverse faults in the Gediz Graben is documented for the first time here. Fault data suggest an approximately N–S direction of compression that has governed the contractional deformation. Yet the limited distribution of these structures prevents to relate them with confidence to a regional deformation phase.

Extensional folds occur in association with normal faults either as structures longitudinal or transverse with respect to the general graben trend. Transverse folds are a very common within the buried graben block, owing to the lateral displacement gradients (lateral difference in offset) on the individual fault segments along the southern margin of the graben. Synclines and anticlines have formed at displacement maxima and minima, respectively. Thickness of strata increases at synclines and decreases at anticlines, thus indicating the syn-depositional origin of the folding.     

煤层割理的形成机理及在煤层气勘探开发评价中的意义

在系统研究鄂尔多斯东缘晚古生代煤层割理的基础上，结合煤化作用和油气生成研究新成果，对煤层割理的形成机理进行了探讨。认为割理是煤化作用过程中，煤因生成水、烃及其它气体而产生收缩内应力和高孔隙流体压力，当其超过煤的力学强度时，致使煤发生张性破裂而形成。割理的原始走向受割理形成时期的古地应力场控制。进而指出中变质光亮煤和半亮煤中割理最发育，因此这些煤层分布区是煤层气勘探开发的优选靶区。     

Changes in sand fractions of Binggou section and the expansion and contraction of the Tengger desert during 50–30 ka

Signs of the evolutionary process are well preserved in the aeolian deposits of desert margins and enable reconstruction of desert expansion and contraction. The sand content (percentage >63 µm) of loess in the loess–desert transitional zone was used as a proxy indicator for determining the proximity of the desert margin. According to the dominant wind direction, generally NW–SE in the northwest Chinese Loess Plateau, a transect was projected to observe spatial changes in sedimentological characteristics of aeolian deposits during the Last Glacial Period. The transect consists of 12 loess sections, starting at Shapotou in the transitional region between the Loess Plateau and the Tengger Desert and ending at Tianshui, which is located at the north foot of the Western Qinling Mountains in the southernmost part of the Loess Plateau. It shows the properties of temporal and spatial distribution of the Malan loess, with reduced sand content from northwest to southeast. A linear correlation model of sand content and distance was obtained, which was similar to the east of the Chinese Loess Plateau. According to this model, and on the basis of optically stimulated luminescence (OSL) dating from Binggou section, a detailed and quantificational expansion and contraction for the Tengger Desert was established. Copyright © 2006 John Wiley & Sons, Ltd.     

基于孔隙胀缩的土−水特征曲线滞后增量模型

土体孔隙比对土?水特征曲线（SWCC）具有重要影响。试验研究表明,土体在经历不同水力荷载路径后,孔隙发生胀缩致使SWCC产生滞后现象。基于这一发现,假设孔隙胀缩可致使SWCC曲线及扫描曲线产生滞后现象,并以轴平移技术为例解释了土体孔隙在水力载荷作用下胀缩的细观行为。在此基础上,将由变截面毛细管模型定义的孔隙等效半径与Fredlund-Xing方程相结合,通过将孔径控制参数?d简化为常量,推导得到了考虑孔隙胀缩并能反映滞后效应的非饱和土SWCC增量方程。该模型仅需通过主干燥及任意一条扫描曲线确定模型参数,即可预测其他扫描曲线。最后,通过5组试验数据验证了该模型对不同类型土的适用性且该模型具有预测高阶扫描曲线的能力。