黄鼠冬眠和活跃状态心肌钙调节的实验分析

研究了冬眠状态黄鼠与活跃状态黄鼠心肌在Rynodine，CD^2 和低[Na ]。作用下动作电位和收缩力的变化。实验表明黄鼠能随活动状态的不同而改变钙调节方式，在冬眠状态主要通过增强内源钙的利用进行钙调节。     

可生物降解高吸水材料的制备以及制备工艺对吸水倍率的影响

以淀粉为原料，采用反相悬浮聚合方法，通过研究交联反应时反应时间、搅拌速度、反应温度以及催化剂质量分数、交联剂质量分数、淀粉质量分数和分散剂质量分数一系列工艺条件制备出可完全生物降解的高吸水材料，通过测定高吸水材料的吸水倍率揭示出制备工艺对可生物降解高吸水材料吸水倍率的影响规律。     

船舶海水管系的腐蚀及其防护

论述了船舶海水管系腐蚀的主要原因及影响腐蚀的重要因素，提出了防止管系腐蚀的方法。     

工业裂解炉数学模拟的加速算法

乙烯裂解炉裂解过程模拟是一个复杂的迭代试算过程 ,现有模拟方法计算时间冗长 ,难以用于在线优化。为此提出的加速算法把裂解过程中的能量平衡关系式作适当简化 ,把反应管管壁温度的求解转换为解一元四次方程的根 ,从而直接得到温度沿管长的微分方程式 ,再结合反应物料和压力沿管长的微分方程式 ,使得裂解过程由一套新的、完整的微分方程组来描述 ,并在模拟过程中对能量关系式的简化作了逐步改进的处理。工业实例表明该算法避免了复杂的迭代计算 ,模拟计算的速度比以前的算法提高约 1/18,同时模拟准确度也有相当的保证     

一种新型的计算机温度检测系统

论述了一种新型的两级总线型电子冷藏箱生产线系统 ,介绍了该系统的技术性能和特点 ,指出了其应用推广的价值     

Loess in the Tian Shan and its implications for the development of the Gurbantunggut Desert and drying of northern Xinjiang

Eolian loess is widely distributed on the various geomorphic surfaces between 700–2400 m a.s.l. on the northern slope of the Tian Shan. It is formed in a synchronous manner with dust transported from the Gurbantunggut Desert in the Junggar Basin. The thickest section of loess was found in the Shawan and Shihezi regions. Paleomagnetic and climatic proxy analyses of over 71 m of a loess-paleosol sequence on the highest terrace of the Qingshui He (River) in the Shawan show that the paleomagnetic Bruhues/Matuyama (B/M) boundary lies at the bottom of paleosol S8, at a depth of 69.5 m, and the bottom of the sequence was estimated to be ∼0.8 Ma. This implies that the extremely dry climatic conditions in the Junggar Basin and the initial Gurbantunggut Desert were present at least by 0.8 Ma. High-resolution grain size series demonstrate that this area and desert expansion experienced two dramatic periods of desert expansions that occurred at ∼0.65 Ma and 0.5 Ma, respectively; and the subsequent continuous enhancement led to the environment presently observed. This tremendous environmental effect, caused by large-scale expansion of the desert and arid region of inner Asia, might be an important driving force for the global temperature drop that occurred in the mid-Pleistocene.     

PGE patterns of ores of Dajing Cu-polymetallic deposit in Linxi County,Inner Mongolia: Indicator to source of metallogenic elements

By comparing PGE patterns of sulfide ores with that of basic-ultrabasic dikes occurring in the Dajing Cu-polymetallic deposit, we discover that there are similar positive slopes between the basic-ultrabasic dikes and the black ores composed mainly of sphalerite and galena, reflecting affinity of their source. The PGE patterns of the yellow ores composed basically of chalcopyrite, arsenopyrite and pyrite are actually different. One is close to the pattern of the mantle lherzolite, and others resemble the pattern of the basic rocks. However, the concentrations of Ru are higher in the yellow ores, reflecting that sulfur attains or approaches saturation in their parent magma. The PGE characteristics of ores and dikes show that the magmas derived from the deep of crust and the metallogenic elements were supplied mainly by growth material of the crust. In addition, the mantle-derived magma also offered some elements.     

Zircon (U-Th)/He thermochronological constraints on Cretaceous thermal extension of Dabieshan orogen

：(U-Th)/He ages of 13 samples from Yuexi-Luotian core and its flanks in Dabieshan orogen fall in the range of 155～85 Ma. He ages for samples from the core range between 85～107 Ma, while those from the flanks range between 114～155 Ma. The result shows that the Yuexi-Luotian core was a thermal dome in Cretaceous with core temperature being much higher than those of the flanks. The thermal extension which resulted in the formation of Dabie core complex lasted until ca. 85 Ma. The magnitude of exhumation in the core is approximately 1528.8 m more than that in the flanks.