峨眉山之雨量

地理位置欲充分了解峨眉多雨之原因必先明瞭其地理位置。峨眉位北纬二十九度二十八分,东经一○三度四十一分,居四川西南部,去省会成都一五0公里.其山自东高起拔海三0七0公尺,山巅高出峨眉县城二公里,在岷江流域     

Analysis of the coupled relationship between grain yields and agricultural labor changes in China

In this paper we establish a model that expresses the coupled relationship between grain yield and agricultural labor changes in China, and present a preliminary discussion of the coupled processes involved in changes in these factors at the county level. Thus, we develop two coefficients on the basis of county-level statistical data for grain yield and agricultural labor for the years 1991, 2000, and 2010, namely, the grain-labor elasticity coefficient (GLEC) and the agricultural labor-transfer effect coefficient (ALTEC). The results of this study show that during the transformation process of agricultural development in China, different kinds of coupled relationships between grain yield and agricultural labor changes co-existed at the same time. For example, between 1991 and 2010, counties characterized by three different coupled modes (i.e., increasing grain yield and decreasing agricultural labor, increasing grain yield and agricultural labor, and decreasing grain yield and agricultural labor) account for 48.85%, 29.11%, and 19.74% of the total across the study area, respectively. Interestingly, a coupled relationship between increasing grain yield and decreasing agricultural labor is mainly concentrated in the traditional farming areas of China, while a coupled relationship between increasing grain yield and agricultural labor is primarily concentrated in pastoral areas and agro-pastoral ecotones in underdeveloped western China. At the same time, a coupled relationship between decreasing grain yield and agricultural labor is concentrated in areas that have experienced a rapid development transition in agriculture, especially the developed southeastern coast of China. The results of this study also show that between 1991 and 2010, 1961 counties experienced a decline in the proportion of agricultural labor; of these, 1452 are also characterized by increasing grain yield, 72.38% of the total. This coupled relationship between grain yield and changes in the proportion of agricultural labor shows a stepped fluctuation and has continually strengthened over time. Data show that mean values for the GLEC and ALTEC increased from–0.25 and–2.93 between 1991 and 2000 to–0.16 and–1.78 between 2000 and 2010, respectively. These changes in GLEC and ALTEC illustrate that the influence of agricultural labor changes on increasing grain yields has gradually diminished. Finally, the results of this study reveal that the ‘Hu Huanyong Line’ is a significant boundary sub-dividing this coupled relationship between grain yield and changes in agricultural labor.     

秦巴山区煌斑岩特征与金成矿的关系

秦巴山区煌斑岩脉广泛分布,岩脉时代主要有加里东期、印支期、燕山-喜山期。大部分含金煌斑岩产于古生代地层中,主要是志留系和泥盆系的细碎屑岩类。本文主要讨论了秦巴山区煌斑岩与金成矿关系,并指出构造破碎作用在成岩成矿中的重要地位。脉体与围岩的同化混染作用、蚀变作用与氧化作用促使金的活化、迁移、富集成矿。     

秦岭地区黄铁矿特征与金矿关系的研究

根据秦岭地区金矿床中黄铁矿特征,总结出典型的微细浸染型和含金石英脉型两种类型矿床特征。黄铁矿与金矿关系密切,含金黄铁矿多产于成矿的富集地段。通过对该区黄铁矿标型特征(晶形、粒级与热电性和微量元素)的系统研究,认为黄铁矿标型特征的研究,对深部找金矿与远景评价具有指导意义。     

中条山胡一篦型铜矿床控矿构造浅析

应用杨赤中滤波法系统分析了胡篦型铜矿几个矿床成矿元素的品位资料,结合矿床地质特征研究,认为该类矿床不仅受ＮＥ向褶皱冲断构造控制,而且还受ＮＷ向断裂构造复合控制,在其交汇部位形成矿柱。矿柱是组成该类矿床的基本单元,其产状与两组构造的交线产状基本一致。     

初议中亚成矿域

给出了中亚成矿域的地质含义与地理范围。此巨型成矿域以发育中、晚元古代及晚古生代成矿作用为其特点。以超大型矿床为重点,并主要围绕金、铜讨论了中亚成矿域6种类型矿床的时空展布。近年取得的进展说明,中亚成矿域在矿产资源优势与潜力方面并不亚于环太平洋成矿域及特提斯成矿域。     

中国东部降水的随机动力预测初步研究

利用一个具有门限的非线性随机动力气候模式,对中国东部江淮流域的降水进行了预报试验。结果表明：模式能对大范围环流降水作出较为准确的形势预报。还比较了海气耦合模式与外强迫模式的预报效果,表明耦合模式的预报效果略好于外强迫模式。     

中国东部降水年际变化的随机动力诊断

利用一个具有门限的非线性随机动力气候模式对中国东部江淮流域的降水进行了分析。结果表明：在不同的门限域中,降水对外部强迫的响应有明显差异,呈现出一定的非线性特征;模式能较好地拟合降水的变化趋势。     

中国近117年年平均气温变化的区域特征研究

用ＲＥＯＦ法以１６０站近４７年的年平均气温变化为依据将我国分为８个年平均气温变化区．以国内及临近国家长资料序列为基础,建立了反映我国各区及全国近１１７年的年平均气温标准化序列．从近１１７年气温变化来看,Ｉ～ＶＩＩ区都有升温趋势,全国平均气温的升温趋势为０．７６℃／１００ａ,北半球陆地则为０．６４℃／１００ａ．最大的为东北,华北、新疆,最小的为四川、贵州．从年代际尺度看我国与北半球陆地的平均气温的变化是相当一致的,相关系数高达０．９３,主要差别在于年际变化．     

秦岭地区砂金分布特征与成矿机理

秦岭地区砂金矿床大部分分布在嘉陵江、汉水及其它们的支流流域。总结了砂金矿床分布特征,并将３种类型进行了对比。系统地对矿源、搬运、储存和富集的成矿模式、成因机理进行了研究。地貌与产构造运动在成矿中占有重要地位。