藏山羊微卫星DNA多态性研究

选用10个SSR标记,经PCR扩增、9%非变性聚丙烯酰胺电泳和银染法显色,对高原型藏山羊、山谷型藏山羊进行遗传多态性研究,并以白玉黑山羊、建昌黑山羊、美姑山羊和新疆山羊作对照.结果表明,10个SSR标记在高原型藏山羊、山谷型藏山羊、白玉黑山羊、建昌黑山羊、美姑山羊和新疆山羊群体的平均H、PIC、Ne分别为0.673/0.631/4.3、0.680/0.649/4.7、0.777/0.660/4.3、0.797/0.716/5.1、0.793/0.561/3.2和0.680/0.629/4.6.高原型藏山羊与山谷型藏山羊(D=0.063)聚为1类;建昌黑山羊和美姑山羊(D=0.026)聚为1类后,再与白玉黑山羊聚为1类;最后两类与新疆山羊聚为1大类,与各群体的来源和生态地理分布一致.     

简述西藏传统的居住习俗文化

文章从西藏民居的基本布局与住房分配、民居装饰、民居修建与礼仪以及民居的类型四个方面论述了西藏传统居住习俗文化的基本内容及其特征。在论述过程中,借助西藏古今居住习俗的实例及其相关研究成果,对西藏传统的居住习俗文化进行了探讨。     

藏文文献数字化保护系统功能测试研究

藏文文献是我国民族古籍中的瑰宝,学术价值很高,对它的数字化保护具有非常重要的意义.功能测试是在已知产品所应具有的功能,通过测试来检测每个功能是否都能正常使用,着眼于程序外部结构、不考虑内部逻辑结构、针对软件界面和软件功能进行测试.     

试探“堆尼玛”和“敖包”的起源

文章通过部分文献资料和实物资料分析“玛尼堆”和“敖包”的起源。笔者认为有关这两种不同文“化象征”的起源涉及远古的中原文化、印度文化、蒙族文化以及藏族文化。藏传佛教在蒙古地区的兴起标志“着血祭敖包”的结束,也标志“着敖包”“和玛尼堆”的另外一种相互包容关系的发展。因此,从某种意义上讲“,敖包”和“玛尼堆”是千古传诵蒙藏民族深深友谊的一种象征与标志。     

嘉庆时期藏兵赴台湾始末探析

嘉庆年间,蔡牵称王台湾,官军屡战屡败,东南海疆危急。嘉庆帝不得不从内陆各地调兵遣将赴台平乱。藏兵因有赴台平定林爽文事变之先例,再次被调遣赴台。藏兵在已陆续开赴台湾过程中,因台湾战事形势逆转,行动也因此终止。但这一行动再次验证了藏兵在清朝军事行动中的重要地位。     

Carbon isotopic records in paleosols over the Pliocene in Northern China: Implication on vegetation development and Tibetan uplift

Carbon isotopic composition of pedogenic carbonate can be used to estimate the proportion of C₄ and C₃ plants. Here we present carbon isotopic data of carbonate in a red earth section at Xifeng, central Loess Plateau. Results show that C₄ vegetation increased in ∼4.4 Ma B.P., stabilized between 4.0 and 3.0 Ma B.P. The character and timing of C₄ expansion on the Loess Plateau are similar, but different with other localities, e.g. Pakistan and Africa, implying that regional climate changes were main factors driving the expansion of C₄ plants. This event is comparable in timing with increased aridity evidenced by Xifeng grain size and North Pacific eolian dust records. Therefore we argue that the Pliocene expansion of C₄ plants in northern China might have been caused by the increased aridity, which in turn might be related to rapid uplift of the Tibetan Plateau.     

鲁西西部壳内物性界面计算及其应用研究

利用位场(重力、航磁)对数功率谱计算了鲁西西部地壳内部的物性(密度、磁性)界面。从资料的处理和结果分析,探讨了本区深层构造的特点和深层构造与浅层构造的关系,并对壳内物性界面的计算结果在能源预测与勘探、地震等方面的应用作了讨论。     

甘南藏族自治州畜牧业产业化发展构想

甘南藏族自治州天然饲草丰富,畜种繁杂,特色突出。在分析畜牧业现状和机遇的基础上,提出了甘南州畜牧资源产业化开发体系构想和产业化经营的对策建议。     

反拱水垫塘底板块上举力变化规律的试验研究

反拱水垫塘是一种新型消能防冲结构,拟在中国溪洛渡等300m级高拱坝中采用,其稳定性是其在高水头、大流量作用下能否安全运用的关键技术之一。结合溪洛渡拱坝,通过模型试验研究了拱坝坝身泄量最大达3万m3/s时,反拱圈横缝止水设施破坏,动水压强贯入底板缝隙,基岩锚固力失效的极端情况下的反拱水垫塘底板块上举力,得出底板块上举力分布规律和脉动上举力谱密度特性,并推算出拱端的极限推力。研究成果对反拱水垫塘设计、运用和稳定研究具有理论和实际意义。     

Elemental composition of aerosols collected in the glacier area on Nyainqêntanglha Range, Tibetan Plateau, during summer monsoon season

In order to investigate the elemental composition in atmospheric aerosols and its sources in the glacier area over the Tibetan Plateau (TP), seven totally suspended particle samples were collected continuously at the col of the Zhadang glacier (30°28′N,90°39′E,5800 m a.s.l.), Nyainqêntanglha Range, southern TP, from June to October 2006. Twenty-seven elements (Li, Be, B, Na, Mg, Al, K, Ca, Sc, Ti, V, Fe, Mn, Zn, Ga, As, Rb, Sr, Y, Cd, Cs, Ba, Tl, Pb, Bi, Th, U) were analyzed by Inductively Coupled Plasma Mass Spectrometry (ICP-MS). The result indicates that the concentrations of most elements (especially crustal elements) are lower than values at the Nam Co Station during the same period of 2005, and also much lower than other sites in the TP such as Wudaoliang and Waliguan. This suggests that elemental compositions of aerosols in the Zhadang glacier area may represent the background levels of the middle/upper troposphere over the TP. Crustal enrichment factors (EFs) reveal that several elements (e.g. B, Zn, As, Cd, Pb and Bi) may have anthropogenic sources. The southern TP is mainly influenced by the summer Indian monsoon during the sampling period. Backward air mass trajectory analysis suggests that air masses in the region may originate from South Asia. Therefore, anthropogenic pollutants from South Asia may be transported by the summer Indian monsoon to the region which clearly affects the atmospheric environment in the southern TP during the summer monsoon season.