贵州温泉水氟研究

氟是机体必须的元素。贵州温泉平均氟含量为1.2mg/l,是贵州地表水、浅层地下水中平均氟含量的21倍。本文通过回归、聚类、对应分析和硫、碳同位素研究得出贵州温泉水氟主要来自寒武系膏盐层的认识。     

茂兰喀斯特山地南方铁杉种群结构和动态初探

基于大小结构分析法、矩阵模型和分布格局距离方法，研究了茂兰喀斯特山地南方铁杉种群的结构和动态特征：①该种群为中衰型种群；②其空间分布格局表现为聚块内个体呈剧烈聚集分布，而聚块个体呈均匀分布；③南方铁杉种群密度（ＤＳ）有随种群个体径级（ＤＧ）增大而增加的趋势：ＤＳ＝０．００３５ＤＧ１．７３２９；④南方铁杉为先锋种群，能于山顶特殊生境中与其它物种一起于一定时期内形成稳定群落，但其终将为阔叶树种取代；⑤在某种程度上，种群的空间分布格局距离法和矩阵模型能够较好地应用于中亚热带森林种群研究．     

论贵州山地高效节约型农业的发展途径及意义

从当代农业的特点、效益出发，结合贵州实际，提出了高效节约型农业研究的５点方向，明确了３个主要技术措施，具有一定的现实指导作用。     

贵州省主要秋粮作物耗水规律的研究

本文把土壤－作物－大气视为一个连续体，应用农田水平平衡方程及人工控制下的大田盆栽试验，分别对贵州省玉米和水稻的总耗水理以及耗水量随时间的变化规律进行了研究。指出省内各地应根据当地干旱气候规律，采取作物合理布局，优化灌溉的必要性。     

贵州毛茛科植物的种类与分布补遗（Ⅱ）

本文为第二报，对贵州毛茛科植物３９种３变种的产地进行了增补，其中梵净山唐松草为新种，小果唐松草，多枝唐松草，网脉唐松草，爪叶乌头，金佛山铁线莲，狭盔高乌头为新记录种和变种，紫鸟头，星毛唐松草为贵州植物志未记载种。     

贵州植物园珍稀濒危蕨类植物

本文介绍引种自贵州各地及我国华中、华东和华东的贵州植物园内的珍稀濒危蕨类植物。除列表表示来源、现状等情况外，还对桫椤Ａｌｓｐｈｉｌａ ｓｐｉｎｕｌｏｓａ （Ｈｏｏｋ）Ｔｒｙｏｎ，扇蕨Ｎｅｏｃｈｅｉｒｏｐｔｅｒｉｓ ｐｌａｍａｔｏｐｅｄａｔａ （Ｂａｋ．）Ｃｈｓｉｓｔ，宽叶水韭Ｉｓｏｅｔｅｓ ｊａｐｏｎｉｃａ Ａ．Ｂｒ．，中华水韭Ｉ．ｓｉｎｅｎｓｉｓ Ｐａｌｍｅｒ和截基盾蕨Ｎｅｏｌｅｐｉｓｏｒｕｓ     

白岩尾矿库初期坝Ⅲ号冲沟斜坡稳定性评价及防渗处理

因变更了初期坝轴线，Ⅲ号冲沟斜坡在清基中发现了隐蔽发育于中厚层白云岩中的卸荷裂隙，裂隙宽度０．１０～１．００ｍ，深度３．２０～４．５０ｍ。根据勘探及试验资料，进行了斜坡稳定性和渗透性评价。结论得出：（１）在天然状态下，Ｋ＞１，斜坡稳定；（２）在饱水状态下，沿ｍ２滑移结构面，Ｋ＜１，斜坡不稳定；（３）斜坡浅层管道式渗透作用，将产生渗透破坏。建议采用团结——帷幕溉浆作防渗处理。     

On emplacement ages of lamproites in Zhenyuan County, Guizhou Province, China

Emplacement ages of lamproites that comprise lamproite and olivine lamproite in Zhenyuan County, Guizhou Province, China, have been constrained by the whole-rock Sm-Nd and Rb-Sr isochron methods and the whole rock K-Ar method. Intrusive activities of lamproites in the Sinantang area of Zhenyuan County, Guizhou Province, took place during the Late Cambrian, as indicated by the Sm-Nd isochron ages ( t ) = (503 ± 17) (2σ) Ma and by the Rb-Sr isochron ages ( t ) = (501.2 ± 4.6) (2σ) Ma. Intrusive activities of olivine lamproites at the Maping with Ⅱ-type diamond and Xitou in Zhenyuan County, Guizhou Province, took place from the Late Cambrian to the Early Ordovician, as evidenced by the Sm-Nd isochron ages ( t ) = (502 ± 27) (2σ) Ma and by the Rb-Sr isochron age ( t ) = (502 ± 27) (2σ) Ma. This suggests that the upwelling hot materials derived from the deep mantle were emplaced from the Late Cambrian to the Early Ordovician (503-497 Ma), while the time terminal of cooling of the geothermal event of magmatism-tectonism probably was at 442.64-435.54 Ma, as dated by the whole rock K-Ar method.     

High resolution stalagmite δ18O records over the past 1000 years from Dongge Cave in Guizhou

Based on MC-ICP-MS U-series dating andstable O-isotope analysis results, a 4-5 years resolution monsoon record over the past 1000 years has been established for two stalagmites from Dongge Cave, Guizhou. The high resolution oxygen isotope record serves as a proxy for variations in rainfall of Asian southwest monsoon over the Yunnan-Guizhou Plateau. A close relation of the δ18O record with the A^14C record from tree rings largely reflects impact of centennial-scale solar activity on the monsoon climate changes. The conspicuous decrease in the δ18O value at AD 1720 indicates an abrupt increase in monsoon rainfall, suggesting that an atmospheric-oceanic couple over the tropical Indian Ocean plays an important role in rapid increase of the Northern Hemisphere temperature over the last century.