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51.
Analysis and simulation of magma mixing processes in 3D   总被引:2,自引:0,他引:2  
D. Perugini  G. Poli  G. D. Gatta 《Lithos》2002,65(3-4):313-330
Magma mixing structures from the lava flow of Lesbos (Greece) are analyzed in three dimensions using a technique that, starting from the serial sections of rock cubes, allows the reconstruction of the spatial distribution of magmas inside rocks. Two main kinds of coexisting structures are observed: (i) “active regions” (AR) in which magmas mix intimately generating wide contact surfaces and (ii) “coherent regions” (CR) of more mafic magma that have a globular shape and do not show large deformations. The intensity of mingling is quantified by calculating both the interfacial area (IA) between interacting magmas and the fractal dimension of the reconstructed structures. Results show that the fractal dimension is linearly correlated with the logarithm of interfacial area allowing discrimination among different intensities of mingling.

The process of mingling of magmas is simulated using a three-dimensional chaotic dynamical system consisting of stretching and folding processes. The intensity of mingling is measured by calculating the interfacial area between interacting magmas and the fractal dimension, as for natural magma mixing structures. Results suggest that, as in the natural case, the fractal dimension is linearly correlated with the logarithm of the interfacial area allowing to conclude that magma mixing can be regarded as a chaotic process.

Since chemical exchange and physical dispersion of one magma inside another by stretching and folding are closely related, we performed coupled numerical simulations of chaotic advection and chemical diffusion in three dimensions. Our analysis reveals the occurrence in the same system of “active mixing regions” and “coherent regions” analogous to those observed in nature. We will show that the dynamic processes are able to generate magmas with wide spatial heterogeneity related to the occurrence of magmatic enclaves inside host rocks in both plutonic and volcanic environments.  相似文献   

52.
Based on cross-dating tree rings from the Tianmu Mountain, Zhejiang Province, the tree rings α-cellulose δ 13C time series was measured. By spectrum analysis, the variation of tree-ring δ13C sequence shows a quasi periodicity of 4.4 years, which is coincident with the standard cycle of El Nino. After removing the long-term decrease trend of the δ13C variation related to atmospheric CO2 concentration, the response of the δ13C to climate elements was analyzed using meteorology data from a nearby weather station. The results suggest that there is a distinct relativity between high-frequency variation of tree ring δ 13C series and seasonal climate parameters, e.g. Temperature and precipitation, with a significant time-lag effect. In addition, the high frequency also reflects the strength change of the East Asian Monsoon. The multiple regression method was employed to reconstruct the historical climate, and to analyze the climate change and trend in the last 160 years in the northern Zhejiang Province.  相似文献   
53.
螺旋CT三维重建在骨盆骨折中的应用   总被引:2,自引:0,他引:2  
目的:探讨用螺旋CT三维重建评价骨盆骨折的临床应用价值。方法:收集骨盆骨折17例,采用螺旋CT三维重建检查。结果:17例检查均取得清晰立体图像,且可消除某一骨性结构,单独观察骨盆某一组成骨的骨折情况。结论:螺旋CT三维重建在骨盆骨折的诊断、手术方案的设计及教学等有较高价值。  相似文献   
54.
吕建华  季劲钧 《大气科学》2002,26(2):255-262
利用大气-植被相互作用模式AVIM对青藏高原上30个站点进行模拟计算,给出了青藏高原上植被叶面积指数和净初级生产力的分布特征。模拟结果表明,高原上叶面积指数、净初级生产力由东南向西北减少,模拟和观测的分布相一致。分析指出,青藏高原净初级生产力的分布决定于水热条件的共同作用,降水充沛、温度适宜的青藏高原东南部净初级生产力较高,而青藏高原西北部由于降水过少或温度过低,初级生产力很低。  相似文献   
55.
By measuring Sr/Ca ratios of the ostracod shells (Limnocthere cf. inopinata) in sediments of the Daihai Lake, and combined with Sr2+/Ca2+ ratios of the lake water, this paper obtained paleosalinity of the lake water. Vaporizing experiment of the lake water in laboratory showed that there was a quantitative relationship between salinity and oxygen isotope. Using this relationship, oxygen isotope values of the paleo-lake water were calculated. By measuring the oxygen isotope of the authigenic carbonate in the lake’s sediments, and in combination with the oxygen isotope values of the paleo-lake water, the paleotemperature of the lake water was calculated. Finally, based on these proxies, the paleoclimate in the lake basin was explored.  相似文献   
56.
中国耕地有机质含量变化对土地生产力影响的定量研究   总被引:23,自引:6,他引:23  
王卫  李秀彬 《地理科学》2002,22(1):24-28
在土地持续利用与管理研究中,土地质量变化对土地生产力影响的定量研究是核心内容之一。借助新古典经济学的生产函数法,构建了我国耕地的生产函数模型,定量模拟了我国耕地有机质含量变化的边际产出率性和边际生产力。初步结果表明,由于我国长期存在耕过度利用导致有机质含量及肥力下降问题,当前提高耕地质量的增产潜力十分可观。  相似文献   
57.
阜新矿区地面塌陷灾害对土地生产力的影响   总被引:16,自引:0,他引:16  
在研究地面塌陷对一个地区的影响时,一般只侧重于其对建筑物、铁路的影响,而对土地生产力影响的探讨和研究还不够深入。对于阜新矿区来说,地面塌陷对该区土地生产力的影响更是空白,前期的工作仅仅侧重于地面塌陷的调查,如果就地面塌陷对土地生产力的影响做一决的概括和分析,无疑会给今后治理由地面塌陷带来的灾害提供借鉴作用。本文结合大量实测、实算数据,应用土地复理论与方法对地面塌陷引起的土地侵蚀、土壤盐碱化、土壤湿度、土壤质量水平等四个方面做了较为系统的阐述,并对灾害的治理提出了见解。  相似文献   
58.
Multi-parameter studies (stable isotopes in carbonate and organic matter, pigment,organic carbon and nitrogen contents) from a 660-yr continuous sediment core from Lake Cheng-hai, a closed, eutropic lake in southern China, provide information on lake historical eutrophi-cation. During the last 660 years, great changes have taken place in productivity and eutrophi-cation of Lake Chenghai in response to human activities. In 1690, the productivity of the lakebegan to increase as Lake Chenghai became closed from agriculture in the lake‘‘ s watershed. In 1942, Lake Chenghai evolved to eutrophic state, marked by an increase in organic carbon, ni-trogen, CaC03, pigment contents and obvious negative values of stable isotopes, which is more or less simultaneous with the large-scale population immigration during the period. In 1984, in-tensive human activities induced modern lacustrine productivity and eutrophic level. Human-in-duced trophic changes during the past few decades have affected the Lake Chenghai ecosystem tosuch an extent that it has never experienced before in the last 660 years.  相似文献   
59.
黄土湿陷性的微结构不平衡吸力成因论   总被引:16,自引:0,他引:16  
分析了黄土粒间吸力的基本特性及其湿陷的微观过程,探讨了黄土在应力状态作用下由于浸水增湿而产生的微结构单元体滑移动力和阻力随饱和度、上覆土压力的变化规律,提出了微结构与广义吸力综合效应的湿陷性控制机理---微结构不平衡吸力成因论及其定量模型,从理论上分析了湿陷性与增湿水量、压力及深度的关系,揭示了土湿陷效应的内在规律。文中认为,湿陷过程就是水的楔入导致小孔隙广义吸力的逐渐丧失和大孔隙湿吸力的逐渐增大引起的微结构重建动力与重建阻力间的动态对抗过程。最后,讨论了湿陷的基本条件及影响因素。  相似文献   
60.
Mapgis在地质学中的应用   总被引:7,自引:0,他引:7  
简要讨论了Mapgis的主要功能,重点阐述了Mapgis的地质制图技术、空间分析技术以及二次开发能力在地质学领域中的应用,并举例论述之。Mapgis的地质制图技术将纷繁复杂的传统地质制图过程简化,而且美观精确;空间分析技术可以将矢量数据和栅格数据综合制作出各种图形和图象文件,方便分析;地质工作者也可以运用Mapgis的二次开发能力来开发面向特定领域的系统。  相似文献   
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