陕西强震(M≥6)的统计研究

本文用概率统计方法对陕西强震(M≥6)的时段求出理论分布函数,找出了关中强震时段的周期和多项式,并讨论了转移状态.     

再论周期表中的相对论性效应

简要地论述了多电子原子体系的主要相对论性效应,即相对论性收缩、自旋-轨道分裂和相对论性自洽扩展等。随着元素原子序数增加,上述效应的影响迅速增大,这是决定重元素及其化合物“反常现象”的主要因素。诸如某些重金属元素的“反常性”、特殊性、差异性和相似性均可用相对论性效应予以解释。     

关于中国气候地貌若干问题的探讨

本文主要以冰川冻土地貌、岩溶地貌及相应的黄土堆积、红土的发育等地貌与堆积物以及海面与湖面变化、生物群演替与迁移等多种气候标志为依据,讨论我国气候地貌形态特征、分布规律、发育深度等问题,进而探讨我国第四纪以来气候变化总趋势。     

北部湾海槽中全新世以来气候变化与重金属积累关系

【目的】为了探寻北部湾湾口重金属沉积规律,研究中全新世以来该地区海槽重金属分布、累积及联系。【方法】在北部湾南部海槽处钻取200cm长度岩芯进行垂直分样,并对典型重金属Pb、Cr、Zn,微量元素,粒度,矿物,14 C定年等指标进行综合测试及分析。【结果】岩芯沉积物的化学蚀变指标CIA显示,气候波动变化,总体上气候趋向暖湿,陆源供给加大,可分为两个基本气候阶段;重金属具有陆源性,且细粒级与重金属对气候波动响应明显,含量随深度变浅,即随气候演进而呈增加趋势;岩芯沉积物组分以悬移质为主,与海水悬移质粒级有对应性,其中重金属来自吸附与再沉积,6~9φ为吸附粒级;重金属积累系数fa变化曲线显示,重金属自25cm以来积累加快,Pb的相对斜率增加且分化明显。【结论】重金属含量变化是对气候波动的响应,晚全新世后期重金属(尤其是Pb)积累有加快趋势,可能与人类活动有关。     

土壤与植物生态化学计量学研究进展

生态化学计量学是一门新兴科学,主要研究生态作用和生态过程中能量平衡及碳、氮、磷等多重化学元素的平衡,有机统一了生物学不同层次(分子、细胞、个体、种群、生态系统以及全球尺度)的研究理论。陆地生态系统的生态化学计量学研究具有重要意义,土壤和植物的碳、氮、磷比例关系可以表征生态系统的养分限制状况以及有机质的分解程度及其对土壤肥力的潜在贡献等。主要综述了生态化学计量学的概念、起源及研究简史,重点概述了陆地生态系统(主要为草原生态系统)中土壤与植物碳、氮、磷的生态化学计量学特征及其对气候因子及人为干扰等因素的响应。     

太行山大峡谷与长子木化石的地质时期气候现象浅探

在分析、介绍太行山大峡谷、长子木化石地质结构基础上,探讨了太行山大峡谷与长子木化石的地质时期气候现象,提出了大峡谷与木化石群形成时期基本一致的结论。     

朔城区2009年马铃薯产量与气候特点的关系

综述了朔城区马铃薯作物在各个生育期对气候条件的要求,通过分析2009年马铃薯生育期的气候特点,进一步探索了气候条件与作物产量的相关性,总结了异常气候条件对马铃薯产量的影响,以期为指导种植马铃薯提供趋利避害的依据。     

Climatic variations recorded by the sediments from Erhai Lake, Yunnan Province, southwest China during the past 8000 a

Erhai Lake is a large lake with important climatic significance in Yunnan Province, southwest China. The multi-proxy sedimentary records from Erhai Lake indicate the 9 stages of climatic changes with the alternation of warm-dry and cool-wet during the past 8000 a. The variations of Asian monsoon systems were the main cause for the climatic changes in southwest China. The warm-dry period was coincident with the intensification of India monsoon and Northwest Pacific Sub-tropical High Pressure, and the cool-wet corresponding to weak of India monsoon and its main rain belt moving back to southwest China.     

Loess buried paleosols geosols welded paleosols pedocomplexes towards a global quaternary pedostratigraphy and paleoclimatic history

Micromorphological studies show that a comparision of the loess-paleosol sequence of the Karamaydan section, Central Asia, with the upper part of the Luochuan section, China, clearly indicates that for the Brunhes chron the sequence at Karamaydan is even more detailed than the corresponding section at Luochuan. Single paleosols at Luochuan correspond to pedocomplexes at Karamaydan; some pedocomplexes at Luochuan are represented by more detailed successions at Karamaydan (fig. 1). The loess-paleosol sequence at Karamaydan should therefore be regarded as a key sequence for reconstructing the climatic history of the Brunhes epoch. Correlation with the deep-sea oxygen isotope record of Bassinot et al. (1994), which includes an accurate astronomical time scale, allows a detailed chronostratigraphical subdivision of the loess-paleosol sequence in Karamaydan for the Brunhes chron. Mineralogical and clay mineralogical investigations show that there is little difference in the type and amount of pedogenic clay mineral formation between two Holocene soils and the paleosols in the Brunhes chron at Karamaydan. These results indicate that the climates of the interglacials represented by the B or Bt horizons of the buried paleosols were similar to that of the Holocene. In view of these results the Paleopedology Commission should develop a uniform terminology of mono- and polygenetic paleosols and pedostratigraphic units which can be used globally.