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The external scale of cobalt sulfide and yttrium oxide-surfide particles in the inner scale were found respectively after corrasion in Pa .!$+ lo-'' Pa Q. Beneath the external scale, a region of internal sulfidation-oxidation of yttrium was also present. The comion pduct in lo-' Pa .!$+ 10-l5 Pa Q was only a very thin surface layer of yttrium oxysulfide and an internal oxidation zone of yttrium.

并有助于降低纯Co的腐蚀速率,10^02Pa硫压下,合金表面形成的腐蚀产物为多层、以为硫化钴,中间层为由两金属化合物怕成分复杂的混合物层,最内层是由氧和硫引起的Y的内腐蚀区;在10^-3Pa硫压下,合金没有形成外层硫钴,仅在表面形成较薄的Y的硫氧化物,其下为Y的内氧化区。

All iliac hone graft fused well and a great deal of bony callus was found the vertebral body surface. Lucency area was in seen surrounding the hone graft, titanium and AC-AFF on the X-ray films, and there wan new bone formation in the interface of internal union and bone. The central region of titanium and AC-AFF became vague and new bone formation was found in the intracavitary aim of implants by CT scan. And port of the new hone transited the parietal reticulation and connected with normal ones at titanium and AC-AFF.

髂骨植骨组融合情况良好,融合界面上有较多的骨痂生成。X线摄片见植骨块、钛网、AC-AFF中空区域模糊且有骨组织生长,内植物周围无透光带存在,植骨界面上有骨桥形成;CT扫描在钛网及AC-AFF组可见内植物腔内形成的新骨通过其四壁的网眼结构与周围骨质相接,说明所有标本均达到骨性融合,但其中以AC-AFF组形成的新骨数量为多,且较为成熟。

One or more plane sections (8,9) and part cylinders (10,11) connecting to the plane sections (8,9) are formed at the outside (7) of the capillary using for fixing the fiber, all the part cylinders (10,11) are formed with a single center axis and the same radius, meanwhile a patchhole (3) of the inserting fixed fiber (2) is formed in the deflected position of the center axis and in the vertical direction of the first plane section (8) which is used as the standard.

在光纤固定用玻璃毛细管(1)的外面(7)形成有一个或多个平面部(8、9)和与该平面部(8、9)连接的一个或多个局部圆筒面(10、11),该所有的局部圆筒面(10、11)都是以单一的中心轴和相同半径形成的,同时在与作为基准的第一平面部(8)垂直的方向上从中心轴偏离的位置上形成有插入固定光纤(2)的插入孔(3)。

Because of the gradually advancing, the traditional Wushus cultural system took shape in the activity in traditional Wushu culture and education, makes its education pass the characteristic with advancing gradually of forming of the activity content on, have formed its basic shape of regarding passing on in the clan , schism and sectionalize

在传统武术文化教育传承活动中,由于传统武术文化体系形成的渐进性,使其教育传承活动内容的形成具备了渐进性的特征,并形成了以宗族、宗派和门户性教育传承为其基本形态,以师徒传承为其基本传承方式,以武德教育为其传承核心,以武术私学教育为其主体教学活动的一系列特征。

The formation of silique dehsicence susceptibility was investigated in terms of water content, synthetic rate of ethylene, enzyme activity of exo polygalacturonase and end cellulase , cell alteration in dehiscence zone in silique and silique dehiscence susceptibility during silique development.

从油菜角果发育过程中角果含水量、乙烯合成速率、外切 PG 酶和内切纤维素酶活性,以及角果裂区切片观察等方面研究了角果开裂敏感性形成的原因⒚花后50d 的角果果柄端壳状果瓣和线状果瓣间的裂区薄壁细胞膨大,在高倍光学显微镜下可见胞间空隙开始形成⒚此前6d 内乙烯合成速率迅速上升并出现第二次合成高峰,与之同步发生外切 PG酶和内切纤维素酶活性急剧上升,而乙烯合成第二高峰出现于角果含水量低于80%以下⒚由此看来,角果失水引起乙烯合成第二高峰出现,从而导致水解酶活性上升,最终导致果瓣裂区薄壁细胞膨大,分离和胞间空隙形成及角果开裂敏感性产生

They were able to find a mathematical formula that applies to both the formation of icicles and the formation of stalactites, which look just like icicles but are formed by the accumulation of minerals dissolved in water dripping from the roofs of caves.

他们还发现,一个数学公式,既适用于形成的冰柱和形成钟乳石,看起来就像冰柱但所形成的积累,矿物溶解在滴水的屋顶洞穴。

The crystallization temperature and pressure of clinopyroxene phenocrysts from the ankaramite and basalt were estimated on the basis of the clinopyroxene-melt equilibrium principle: 1345~1366℃ and 1.75~2.05Gpa for ankaramite, with average geothermal gradient of 20-24℃/km, suggesting anomalous heat or geothermal gradient in this region may be one of the key reasons to produce the porphyry copper deposits in the region. In contrast, those in the basalts fomed under a relatively low crystallization temperature (1129~1191℃), and the pressure (1.19~1.60Gpa) and depth (39~53km), suggesting that the basalt formed under a condition of lower temperature and pressure.

根据单斜辉石-熔体平衡原理计算了富辉橄玄岩和玄武岩中斑晶相辉石形成的温度和压力,前者变化范围主要集中在1345~1366℃和1.75~2.05GPa,其深度相当于58-67km,平均的地温梯度大约20~24℃/km,说明该区具有异常的热或地温梯度,这可能是导致本区斑岩铜矿形成的主要原因之一;后者的温度和压力都相对较低,分别为1129~1191℃和1.19~1.60Gpa,而相应的深度为39~53km,暗示着玄武岩是在相对低温低压的环境中形成的演化岩浆。

ObjectiveNon-heparinized autohemic arterial blood of the rat was injected into its caudate nucleus to establish a model of intracerebral hemorrhage. The changes of edema in various regions of the brain were measured at different time after hemorrhage. Meanwhile, the effects of erythrocytes and thrombin on the formation of cerebral edema after cerebral hemorrhage were studied to explore the pathophysiological mechanism of cerebral edema and the roles of erythrocytes and thrombin in this process.

目的 利用自体未肝素化新鲜血回注法建立大鼠尾状核出血模型,观察脑出血后不同时间不同部位脑组织水分含量的变化,并分别研究红细胞、凝血酶对脑出血后脑水肿形成的影响,揭示脑出血后脑水肿形成的病理生理机制,并阐明红细胞、凝血酶在脑出血后脑水肿形成中的作用,从而为临床脑出血病人病情评估及治疗提供理论依据。

Brought forward and reasoned the forming mechanism of Maowusu sandy land. Based on the analysis of the development of Holocene rivers and related loess and windsandy geomorphology, the paper put forward the forming mechanism of Maowusu sandy land as follows: while the climate became dry, the exterior channels extended backwardly and cut through the remained lake system of ancient Hetao lake. This resulted in the rapid discharge of underground water. The vegetation living on this water resource was destroyed completely. Then the sand began to form.

对毛乌素沙地的形成机制进行了新的探索基于对过渡地带全新世河流及其相关的黄土和风沙地貌发育、土地利用变化等分析,提出毛乌素沙地的形成机制:在气候变干的同时,外流河谷溯源延伸,切穿了长城以北河套古湖残遗湖系,使地表地下水迅速外泄,原靠湖系水资源维系的生长在河套古湖湖滨沙堤形成的沙地上的非地带植被的生存条件被彻底摧毁,而起沙。

The results show that these gravel silty clays distributed at the range between the rock slope with an altitude lower than 190m and the rock platform with an altitude about 140-150m are formed from sliding; and that those gravel silty clays distributed above 190m of the rock surface are residual, colluvial and talus deposits; and that the gravel sand layer located along Zhuxi River is a kind of alluvial deposit.

研究结果表明:分布在基岩面高程190m以下的斜坡与基岩面高程140~150m平台上的粉质黏土夹碎石土层是由滑坡作用形成的;分布在基岩面高程190m以上的粉质黏土夹碎石土层是由崩积、残积及坡积作用形成的;卵石砂土层是苎溪河的冲积作用形成的。

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