江苏省宁镇扬山地丘陵地区农业资源的综合开发利用

宁镇扬山地丘陵地区土地面积133.9万公顷,农业资源丰富,是江苏省开发潜力很大的地区之一。本文从气候资源、水资源、土地资源和生物资源,阐述了它们的区域优势;探讨了农业资源开发利用中的主要问题。提出了综合开发利用的建议和对策,制定农业资源综合开发的总体规划;建立农业资源综合开发治理试验区;发挥山丘地区资源优势,建立商品生产基地。     

龙门山及其邻区的构造和地震活动及动力学

论述了龙门山推覆构造带、岷山隆起、成都平原和龙泉山地区的构造和地震活动，讨论了构造活动特点和演化历史，并分析了它们的形成机制和动力学问题     

大别山北麓石炭系研究新进展

研究区石炭系属残留海盆沉积。在固始柳林泥盆纪（？）花园墙组上部首次发现社内期Ｄｉｂｏｌｉｓｐｏｒｉｔｅｓｄｉｓｔｉｎｃｔｕｓ－Ａｕｒｏｒａｓｐｏｒａｍａｃｒａ孢子组合，据此建立固始组。上覆大杨山组为典型磨拉石建造，推论造山运动发生于中、晚泥盆世。杨山组植物组合的特点似显示在早石炭世末华北、华南板块已互相接近，局部地段可能已拼合。     

Isotopic studies for the rational use of water resources in the front plain of Tianshan Mountain

Based on the analysis of the environmental isotopes of about 100 water samples, the waters in the front plain of the Tainshan Mountain are divided into eight subprovinces on a horizontal plane and four zones in a vertical plane. The characteristics of the recharge, runoff, and water storage of different waters are discussed, and the runoffs in several sections are also calculated. Last, the tentative space-time regulation plan of the water resources is presented on the basis of the study of the environmental isotopes.     

桐柏山花岗岩类Pb、O、Sr同位素特征

本文首次对桐柏山花岗岩类的Ｐｂ、Ｏ、Ｓｒ同位素进行研究。其长石铅同位素组成是２０４Ｐｂ＝１．４００（１．３８９－１．４１１），２０６Ｐｂ／２０４Ｐｂ＝１７．１４８（１６．８４７－１７．４３８），２０７Ｐｂ／２０４Ｐｂ＝１５．４２８（１５．３７８－１５．４８４），２０８Ｐｂ／２０４Ｐｂ＝３７．８８６（３７．５８３－３８．２９６）。与邻区花岗岩类相比，基本相当于胶东地区。全岩矿δ１８Ｏ＝８．４８（７．４９－９．３７）。８７Ｓｒ／８６Ｓｒ（ｉ）＝０．７０９０（０．７０６４－０．７１３８）。这些数据结合岩石矿物特征表明，本区花岗岩类的成因类型属Ⅰ型或同熔型。铅同位素组成揭示本区大地构造可能归属华北地台。     

山地降水垂直分布模式计算方法的改进

以傅抱璞公式为出发点，直接对抛物线进行二次响应面回归，计算简便、精确度高；同时还对山地降水高斯模式进行了简化，并将其应用于黄山降水分析中，效果较好。     

大别山马鬃岭蕨类植物资源的开发利用

马鬃岭自然保护区共有蕨类植物２８科、５５属、８９种，本文论述了马鬃岭蕨类植物的基本特点和分布规律，并根据用途将区内的野生蕨类植物划分为７类，即药用资源、观赏资源、工业原料资源、指示资源、食用资源、编织和包装资源、饲料和绿肥资源。文章最后提出了合理开发利用马鬃岭蕨类植物资源的一系列建议。     

山岳风景区客流研究：以安徽黄山为例

山岳风景区在我国旅游资源中占有重要地位，已有相当规模的客流量。因此，山岳风景区客流研究重要性日趋明显。笔者以安徽黄山为例，进行山岳风景区客流基本规律研究，揭示了山岳风景区客流时空分布的基本特征；预测了未来客流规模；探讨了客流对旅游环境的影响；提出了山岳风景区旅游发展的基本思路。     

Human impacts to mountain streams

Mountain streams are here defined as channel networks within mountainous regions of the world. This definition encompasses tremendous diversity of physical and biological conditions, as well as history of land use. Human effects on mountain streams may result from activities undertaken within the stream channel that directly alter channel geometry, the dynamics of water and sediment movement, contaminants in the stream, or aquatic and riparian communities. Examples include channelization, construction of grade-control structures or check dams, removal of beavers, and placer mining. Human effects can also result from activities within the watershed that indirectly affect streams by altering the movement of water, sediment, and contaminants into the channel. Deforestation, cropping, grazing, land drainage, and urbanization are among the land uses that indirectly alter stream processes. An overview of the relative intensity of human impacts to mountain streams is provided by a table summarizing human effects on each of the major mountainous regions with respect to five categories: flow regulation, biotic integrity, water pollution, channel alteration, and land use. This table indicates that very few mountains have streams not at least moderately affected by land use. The least affected mountainous regions are those at very high or very low latitudes, although our scientific ignorance of conditions in low-latitude mountains in particular means that streams in these mountains might be more altered than is widely recognized. Four case studies from northern Sweden (arctic region), Colorado Front Range (semiarid temperate region), Swiss Alps (humid temperate region), and Papua New Guinea (humid tropics) are also used to explore in detail the history and effects on rivers of human activities in mountainous regions. The overview and case studies indicate that mountain streams must be managed with particular attention to upstream/downstream connections, hillslope/channel connections, process domains, physical and ecological roles of disturbance, and stream resilience.