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There are 8.6%~10.91% foreign matter in the sphenes, in which radioactive elements of strontium, cesium and uranium range from 4.26% to 4.58%. The change of structural cell parameters of sphenes is still very little,Δa=-0.0009 nm~0.0041 nm,Δb=0.0018 nm~0.0004 nm,Δc=0.0002 nm~0.0048 nm,Δβ=-0.10°~0.09° with high crystallinity of 99.27%~96.46%. Though, the age of sphene from the Fenghuang Mountain is about 1000 Ma, and experienced 775 Ma~1758 Ma geological evolvement and alpha decay, its crystallinity only decreased 3%, and its crystal shape and structure are still fine, indicating that sphene is of good ability to solidify radioactive elements. Therefore, sphenes are ideal minerals for solidifying nucleus waste.

通过对北祁连牛心山变质杂岩体中榍石(775Ma)和山西凤凰山花岗岩中榍石(1758Ma)的XRD及EDS等测试与研究,结果表明:两地榍石的杂质元素质量分数高达8.6%~10.91%,放射性核素锶、铯和铀的质量分数达4.26%~4.58%;晶胞参数的变化极小,△a=-0.0009nm~0.0041nm、△b=0.0018nm~0.0004nm、△c=0.0002nm~-0.0048nm、△β=-0.10°~0.09°,结晶度仍高达99.27%~96.46%,榍石经过10×10^8a的地质作用,结晶度仅减少了3%,显示榍石固化放射性系列核素的能力较强,虽经历了约775Ma~1758Ma的复杂地质演化及其所含放射性核素的衰变作用,其晶体结构完好,稳定性极高,是值得期待的理想核废物固化矿物。

At the same time, the ballistic limit curves of the Whipple shield in a velocity range from 0.5 km/s to 5.5 km/s was obtained. Comparing to the predicted curve from Christiansen ballistic limit equation, the experimental minimum critical projectile diameter is slightly greater than the prediction.

通过固定弹丸直径,改变弹丸撞击速度,寻找临界撞击速度的方法获得了铝合金Whipple防护结构在0.5~5.5 km/s撞击速度区间内的撞击极限曲线,并与由Christiansen撞击极限方程得到的撞击极限曲线进行了比较,结果表明,实验最小临界弹丸直径略大于预测值。

The determined thermal conductivity values vary from 0882 to 678 W/m?K and the calculated heat flow values in Jianghan Basin range from 419 to 609 mW/m2,with a average of 523 mW/m2.It shows that the influence of tectonothermal event before Cenozoic in Jianghan Basin has faded away,and the basin has cooled down.

结果显示江汉盆地热流419~609 mW/m2,平均523 mW/m2,盆地总体表现为较低的大地热流,反映了中新生代以来构造活动逐渐减弱,盆地不断冷却的结果;从盆地内热流分布看,热流分布南高北低,反映了江汉盆地构造活动的不均一性。

The model is valid for devices with channel length varying from 30 μm to 6 μm while channel width is 6 μm under a temperature range from 298 K to 343 K.

此载子传输模型在元件通道长度30 μm - 6 μm,通道宽度为6 μm时,温度从298 K变化到343 K下,皆能正确的描述出元件的特性。

40Ar/39Ar data of quartz from the granite porphyry and from the quartz veins in the granite porphyry range from 187.87±1.53Ma to 244.88±2.48 Ma, indicating products of structural hydrothermal fluids of Late Hercynian, Indosinian or Early Yanshanian perods.

花岗斑岩和花岗斑岩内的石英脉体中石英样品的40Ar/39Ar年龄数据表明户,40Ar/39Ar坪年龄值在187.87±1.53 Ma至244.88±2.48 Ma之间,是加里东期花岗斑岩成岩作用之后,海西、印支或者燕山早期多期构造热液作用的产物。

Heat-treating within the temperatures range 700 to 800℃, the transition temperature of heat-treated C-glass became higher with increasing heat-treatment temperatures and gradually approached the transition temperature of the B-glass without TiO〓; the appearance of the C-glass gradually changed from brown-violet colour to intense blue-violet colour and even to opalescence; and the phase separation morphology of TiO〓-rich phase gradually changed from an interconnected phase to a siliceous droplet phase embedded in SiO〓-rach matrix phase with increasing the heat-treatment temperatures.

在玻璃的转变点附近的温度范围内热处理含TiO〓系统玻璃时,随热处理温度的升高,玻璃的转变温度增大,逐渐向不含TiO〓的MgO-Al〓O〓-SiO〓系统玻璃的转变温度靠近;玻璃的颜色逐渐由紫色向兰色及乳白色转化,这是分相玻璃中两相组成在热处理过程中的变化所引起的。

The cultural condition of PGPR strains Temperature,pH,light,cultural method,acid or alkali producing,and salt tolerance of 9 PGPR strains isolated from Gramineous Forage were tested,the results showed that all the PGPR strains could grow in the temperature range from 5℃~45℃,and optimum temperature for 178,O-6,Dry6 strains was 35℃,for X5,173,Y5,C-6 strains was 30℃,for N4 strain was 25℃~35℃,for 86 strain was 25℃;most of PGPR strains prefered to neutral or alkaline condition,strains 178,O-6,N4 and X5 were preferable to alkali condition especially;light was beneficial to PGPR's growth;all of them produce alkali;most of PGPR strains were not sensitive to NaCl concentration;all the strains were aerobiotic bacteria.

结果表明:各供试菌株对温度的适应范围较广,在5℃~45℃范围内均能生长,178、O-6、Dry6 菌株的适宜生长温度为35℃,X5、173、Y5、C-6 菌株的适宜生长温度为30℃,N4 菌株的适宜生长温度为25℃~35℃,86 菌株的适宜生长温度为25℃;大部分菌株在中性或偏碱性的条件下生长好,特别是Dry6、N4 和X5 菌株对碱性环境适应性强,在pH 值8.0 时生长最好;光照有利于菌株的生长;绝大部分菌株在3%NaCl浓度下生长良好,在5%~7% NaCl 浓度下除173 和86 菌株外,其它菌株都能生长,即对盐份的耐受性较好,且9 个菌株均为产碱菌;除173 菌株是兼性厌氧细菌外,其它都是好氧性细菌。

Morphologically similar lesions from 26 patients (mean age, 62 y; range, 46 to 88 y; male/female ratio, 10/16) were retrieved from surgical pathology and consult files. Clinical and endoscopic data were obtained, and immunohistochemistry for S-100 protein, glial fibrillary acidic protein, neurofilament protein, epithelial membrane antigen, claudin-1, CD34, smooth muscle actin, and KIT was performed. The findings were compared with those in mucosal biopsies of 5 submucosal neurofibromas from NF1 patients.

我们从外科病理和档案库里调取了26例病变形态相似的病例(患者平均年龄62岁,范围:46至88岁,男女比例:10/16),得到了他们的临床及内窥镜资料,并给它们都做了S-100蛋白、胶质纤维酸性蛋白、神经丝蛋白、上皮膜抗原、闭合蛋白-1(claudin-1)、CD34、平滑肌肌动蛋白和KIT的免疫组化,所得的结果都与5例NF1患者粘膜下神经纤维瘤的粘膜活检的结果相比较。

The people across Kehjistan appear to range from light brown to very dark skin colors; The Paladin and the Sorcerer appear to be very dark whereas the Sorceress from the Zann Esu Clan appear to be lighter brown.

汉吉斯坦则居住着各种肤色的居民,从亮棕色到暗色;圣骑士和法师都是黑色皮肤,而Zann Esu部族的女法师的肤色则是浅浅的棕色的。

The isolated cells are able to orient and migrate to the magnet in artificial magnetic field but could not orient swimming only under the geomagnetic field. Magnetosomes produced by Acidithiobacillus ferrooxidans were range from 40nm to 90 nm according to the results of TEM. Energy dispersive X-ray analysis indicated that extracted magnetic particles consisted of oxygen and iron. The results show that some Acidithiobacillus ferrooxidans cells have weak magnetotaxis and they could be able to be separated by solid-plate magnetophoresis method from others. With the development of this new isolation method, it is possible that we could do deeper research to generate a comprehensive description of the mechanism that how Acidithiobacillus ferrooxidans synthesize the magnetic particles.

实验结果表明,氧化亚铁硫杆菌具有较弱的趋磁性,在人工磁场下会进行趋磁运动,但仅在地磁场作用下不能定向运动,利用固体平板磁泳筛选纯化含有磁性颗粒的氧化亚铁硫杆菌的方法是切实可行的,磁泳分离技术的进一步完善和改进为传统的微生物菌种分离提供了新的途径,为研究纯氧化亚铁硫杆菌菌株胞内磁性颗粒的形成条件及机理提供了前提条件,也为今后从浸矿细菌中分离筛选更多的含有磁性颗粒的菌株打下基础。

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