The Difference of the Pulmonary-Artery Pressure of the Migrants from Difference Elevation at the 4636 - 4907 m Altitude

Study Objective： To compare and analyze the changes of the pulmonary-artery pressure of the migrants coming from different elevation in the hypoxic environment of 4636 - 4907 m extreme altitude. To explore the susceptibility to hypoxic pulmonary-artery hypertension （PH） in the subjects from different altitude and profession. Methods： By using Color Doppler Ultmsonography （CDU）, measuring the pulmonary-artery pressure of 207 healthy men, who had continuously being lived and worked at the extreme altitude for more than six months, and then were divided into three groups according to their profession and the altitude of original living place. Results： There was a significant difference in the outcomes of pulmonary-artery pressure from the 3 groups. Conclusions： Altitude of original living place, labor intensity are some of factors that impact the pulmonary-artery pressure of the people who exposure to a hypoxic environment. The pulmonary- artery pressure of person without strenuously physical work experience was more sensitive to hypoxic surroundings than that of labor workers. It was not always the fact at an extreme altitude that the moderate altitude mountaineers were superior to other migrants from a lower altitude or plain. The higher PH was found in the groups of the moderate altitude mountaineers and labor workers. It is unlikely certain that one with PH would surfer from HAPE.     

藏药抱茎獐牙菜的胚胎学研究

抱茎獐牙菜（ＳｗｅｒｔｉａｆｒａｎｃｈｉｔｉａｎａＭａｘｉｍ．）花药４室,药壁发育为双子叶型;绒毡层异型起源,为非典型腺质型绒毡层;中层２层;花药壁表皮宿存,与药室内壁一起纤维状加厚．胞质分裂为同时型,四分体的排列方式为四面体型;成熟花粉为２细胞．子房２心皮,１室,８列胚珠,为侧膜胎座．薄珠心,单珠被,倒生胚珠．胚囊发育为蓼型．珠孔受精,受精作用属于有丝分裂前配子体融合类型．胚乳发育为核型．胚胎发育为茄型酸浆Ⅰ变型．反足细胞分裂为５～８个,宿存,每个细胞均多核和异常膨大,反足细胞形成的吸器明显,并在胚乳层之外形成染色深的类似“外胚乳”的结构．果实成熟时,种子只发育至球型胚早期阶段．反足细胞在龙胆科一些高山短命植物中的宿存与分裂具有重要的生殖适应与进化意义,这对于龙胆科一年生植物在青藏高原严酷的环境下,甚至在只有几周的生长季节内完成其生活史是十分重要的     

Melt‐state polymer chain dimensions as a function of temperature

The unperturbed chain dimensions (〈R²〉_o/M) of cis/trans‐1,4‐polyisoprene, a near‐atactic poly(methyl methacrylate), and atactic polyolefins were measured as a function of temperature in the melt state via small‐angle neutron scattering (SANS). The polyolefinic materials were derived from polydienes or polystyrene via hydrogenation or deuteration and represent structures not encountered commercially. The parent polymers were prepared via lithium‐based anionic polymerizations in cyclohexane with, in some cases, a polymer microstructure modifier present. The polyolefins retained the near‐monodisperse molecular weight distributions exhibited by the precursor materials. The melt SANS‐based chain dimension data allowed the evaluation of the temperature coefficients [dln 〈R²〉_o/dT(κ)] for these polymers. The evaluated polymers obeyed the packing length (p)‐based expressions of the plateau modulus, G = kT/np³ (MPa), and the entanglement molecular weight, M_e = ρN_anp³ (g mol^?1), where n_t denotes the number (～21) of entanglement strands in a cube with the dimensions of the reptation tube diameter (d_t) and ρ is the chain density. The product np³ is the displaced volume (V_e) of an entanglement that is also expressible as pd or kT/G. © 2002 Wiley Periodicals, Inc. J Polym Sci Part B: Polym Phys 40: 1768–1776, 2002     

Discovery of the granulite xenoliths in Cenozoic volcanic rocks from Hoh Xil,Tibetan plateau

Two-pyroxene granulite and clinopyroxene granulite xenoliths have been recently discovered in the Late Paleogene toNeogene volcanic rocks (with ages in the range of 4.27～44.60 Ma) that outcropped in Hoh Xil, central Tibetan plateau. Based on theelectron microprobe analysis data, the xenoliths provide constraints for the formation equilibrium temperatures of the two-pyroxene gran-ulite being about 783 to 818℃ as determined by two-pyroxene thermometry and the forming pressure of the clinopyroxene granulite beingabout 0.845 to 0.858 GPa that is equivalent to 27.9～28.3 km depth respectively. It indicates that these granulite xenoliths represent thesamples from the middle part of the thickened Tibetan crust. This discovery is important and significant to making further discussion onthe component and thermal regime of the deep crust of the Tibetan plateau.     

A Study on Forest Species Diversity and Its Ecological Service Function in the Plateau Area of Western Sichuan

This paper presents a study on species diversity and its ecological service function in the plateau area in western Sichuan. The results show that species diversity in the plantations on the cutover land has a tendency to increase and that its ecological service function is to be improved with stand age growing. The species diversity in forest communities is also gradually increased on different succession stage till reaching a climax level. But the species diversity in the climax community is slightly decreased before it reaches a relatively constant status. Ecological service function of diversity is gradually strengthened with the progress of succession. In addition, species diversity in a stand in a similar site and at a same age differs among forest types. Species diversity index within a coniferous and broad-leaved mixed forest is larger than that within a coniferous forest. Meanwhile, species diversity enriches as the tree density increases.     

黄土高原坡耕地生态退耕的植被建设研究--以陕西省黄土高原生态退耕县为例

通过对陕西省黄土高原地区生态退耕县坡耕地的数量、质量调查，指出实现坡耕地退耕的措施?提出在各生态类型区的自然条件下适宜种植的树种、草种和提高植被成活率的途径，分析坡耕地生态退耕后植被建设将带来的经济和生态效益，对整个黄土高原地区的植被建设具有重要的指导作用。     

西藏日喀则地区恰布林组物源分析

长期以来，沿西藏雅鲁藏布江南岸呈东西向展布的恰布林组砾岩，被认为是造山期后磨拉石的产物，而被置于第三纪。由于在屯穷紫色泥岩底部灰绿色粉砂质灰岩中发现腹足类化石Ｋａｔｏｓｉｒａｓｐ．，并结合其他地质证据，可以确定该组时代属于早中侏罗世。结合岩石学特征、典型砾岩中砾石的岩石地球化学和物源区分析表明，恰布林组砾岩的砾石有相当一部分来自蛇绿岩，其特征明显不同于现今的雅鲁藏布江蛇绿岩。因此认为雅鲁藏布江存在早中侏罗世之前的古蛇绿岩。     

黄土高原城市化过程对水土保持的影响

应用系统分析的方法研究了黄土高原城市化的发展趋势和由此带来的城市水土流失的新形式和其危害．提出在黄土高原城市规划和建设中，要积极应对城市化过程造成城市规模的扩大，在城市建设中要建成新的城市功能和体系，要将生活污水、工业污水和排沙分为3大系统，设立环城防护林带，兴建城市不同的功能区，并要完善城市水土保持执法体系，以法规制度来监管防治城市的水土流失．