浙西南环敕木山带畲族妇女“雄冠式”头冠解析

浙西南的环敕木山一带，是畲族迁徙到浙江省境内最早的聚居地，这里的畲族妇女传统“雄冠式”头冠，极具民族特色，整体造型呈三角形，用木、布、银等装饰材料，表现出凤凰吟啭的形态，造型精美，色彩斑斓，蕴含着对祖先图腾的崇敬。通过具体描述其头冠的制作、佩戴方法以及佩戴习俗，力求完整地再现浙西南的环敕木山一带畲族妇女“雄冠式”头冠所承载的畲族文化。     

青海湖旅游区生命周期问题探讨

本文立足青海实际，在分析影响青海湖旅游区生命周期的诸因素基础上，提出了延长该区旅游生命周期的具体措施。     

结合青海实际谈《中国自然地理》的教学

指出青海是祖国十分可爱的地方 ,但是由于地势高峻、交通不便、经济落后 ,因此教育也相对滞后 .文章还对处于经济与教育相对落后的省份 ,青海的高等师范院校应如何上好《中国自然地理》课的问题阐述了看法     

高原鼠兔体重生长动态数学模型之再探讨

本文用麦夸算法构造高原鼠兔体重生长的Logistic和Compertz曲线模型,其结果表明:Logistic曲线比Gompertz曲线更优化,Logistic模型比逻辑斯谛-指要饱和模型的精确度更高.     

青海湖区旅游景点的等级划分及综合评价

本文应用定量与定性相结合的方法，从青海湖区旅游资源的潜力和条件等方面对该景区主要旅游景点进行了综合评价，并提出了旅游业发展的具体构想。     

对青海省高等级公路水资源利用技术的思考

青海省自然环境条件恶劣，公路绿化建设难度大，突出表现在降雨量少且集中、蒸发量大、不同地区分布不均等特点，路侧植物存活与生长困难，建设成效不理想．在降雨量小时起不到补充水分的作用，大雨暴雨时雨水白白流走，并对公路边坡稳定构成威胁．在这样的条件制约下．本研究提出在保护沿线生态环境的前提下，将雨水有效地收集起来，用于公路的植被恢复，既保护了水资源，同时也减少了水害对公路的影响．     

青海城镇体系发展的历史轨迹与动力

青海城镇体系经历了发韧期、奠基期、转型期3个发展历程.在这一过程中,湟水谷地最先拉开了城镇发展的历史帏幕,随后逐步向西扩展进入青海湖地区.宏观上,从农耕区向农牧交错区渗透,进而向游牧区拓展,反映了社会历史进程和地域开发进程的调控作用,因此城镇分布数量和密度呈现出农耕区—农牧交错区—游牧区逐级递减的趋势.中观上,以河流为脉络,城镇发展或溯源而上伸入高原腹地,或向河谷两岸推进,进入山区,表现为从优势生存空间向劣势生存空间的时空转化,城镇数量与密度呈现出川水地区—浅山地区—脑山地区的递减趋势.微观上,河谷农耕区城镇选址多位于河流阶地上,土地肥沃,取水便利;而牧区城镇的选址却往往与水草丰美的牧场相关,映射出古代城镇对自然条件和自然物质基础的依赖性.总体而言,青海省城镇兴起和发展的动力,主要来自于外部中央行政建制和军事据点的设置,而非城镇内部社会经济自我发展.就单个城镇而言,民族文化、民族宗教与民族贸易的亲合关系和响应力,是城镇成长的主要推进剂.     

Critical slope gradient for compulsory abandonment of farmland on the hilly Loess Plateau

Scientific evidence for the upper limit of farmland is proposed. Shallow gully erosion is one of erosion types distributed extensively on sloping farmland in the hilly regions of the Loess Plateau. Field observation and aerial photos interpretation, as well as laboratory experiments show that the shallow gully erosion occurring on the steeper farmland in the hilly regions of the Loess Plateau is an important factor leading to intensive erosion on slope, because of its extensive distribution and intensive runoff collection. The data on the formation, development and distribution of shallow gullies on sloping farmland indicate that critical slope gradient for shallow gully initiation ranges from 15 to 20 degrees with an average of 18.2 degrees. Therefore, it is suggested that critical slope gradient for compulsory abandonment of farmland on the hilly Loess Plateau should be kept within the critical slope gradient for shallow gully initiation to prevent shallow gully formation in order to control soil loss more effectively. But as the first step, the cultivation on the slopes with slope larger than 25 degrees where the maximum erosion occurs should be strictly forbidden.     

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     

Observational study of the circulation in the southern South China Sea

CTD data from two oceanographic survey cruises, conducted by “Shiyan No. 3” R/V during two reversing monsoons, were employed to calculate and analyze the distributions of temperature, salinity and geopotential anomaly in the southern South China Sea (SSCS). Based on these distributions, the horizontal structures of the SSCS circulation are described systematically. Study results show that the SSCS circulation structure could be classified as a two-layer (the upper and the lower) pattern, and that the main circulation in the upper layer (0–400 m) is driven by the South China Sea monsoons and is opposite in direction to the reversal of the monsoons. The distributions of principal current systems and their features are presented. Two important local phenomena, local eddy and oceanic front, were observed.