A tentative 2D thermal model of central India across the Narmada-Son Lineament (NSL)     

《Journal of Asian Earth Sciences》2007,29(4-6):363-371

This work deals with 2D thermal modeling in order to delineate the crustal thermal structure of central India along two Deep Seismic Sounding (DSS) profiles, namely Khajuriakalan–Pulgaon and Ujjan–Mahan, traversing the Narmada-Son-Lineament (NSL) in an almost north–south direction. Knowledge of the crustal structure and P-wave velocity distribution up to the Moho, obtained from DSS studies, has been used for the development of the thermal model. Numerical results reveal that the Moho temperature in this region of central India varies between 500 and 580 °C. The estimated heat flow density value is found to vary between 46 and 49 mW/m². The Curie depth varies between 40 and 42 km and is in close agreement with the Curie depth (40±4 km) estimated from the analysis of MAGSAT data. Based on the present work and previous work, it is suggested that the major part of peninsular India consisting of the Wardha–Pranhita Godavari graben/basin, Bastar craton and the adjoining region of the Narmada Son Lineament between profiles I and III towards the north and northwest of the Bastar craton are characterized with a similar mantle heat flow density value equal to ∼23 mW/m². Variation in surface heat flow density values in these regions are caused by variation in the radioactive heat production and fluid circulation in the upper crustal layer.  相似文献   

GZK cutoff distortion due to the energy error distribution shape     

《Astroparticle Physics》2007,26(6):375-379

The development of an ultra high energy air shower has an intrinsic energy fluctuation due both to the first interaction point and to the cascade development. Here we show that for a given primary energy this fluctuation has a lognormal distribution and thus observations will estimate the primary energy with a lognormal error distribution. We analyze the UHECR energy spectrum convolved with the lognormal energy error and demonstrate that the shape of the error distribution will interfere significantly with the ability to observe features in the spectrum. If the standard deviation of the lognormal error distribution is equal or larger than 0.25, both the shape and the normalization of the measured energy spectra will be modified significantly. As a consequence, the GZK cutoff might be sufficiently smeared as not to be seen (without very high statistics). This result is independent of the power law of the cosmological flux. As a conclusion we show that in order to establish the presence or not of the GZK feature, not only more data are needed but also that the shape of the energy error distribution has to be known well. The high energy tail and the sigma of the approximate lognormal distribution of the error in estimating the energy must be at the minimum set by the physics of showers.  相似文献   

岩石激发极化弛豫时间谱与孔隙结构、渗透率的关系   总被引：11，自引：0，他引：11       下载免费PDF全文

童茂松  李莉  王伟男  范清华  姜亦忠  张加举  丁柱  崔杰 《地球物理学报》2005,48(3):710-716

激发极化衰减曲线包含丰富的地层信息,且由多个指数衰减叠加而成.本文采用奇异值分解法对泥质砂岩的激发极化衰减谱进行多指数反演,得到光滑连续的激发极化弛豫时间谱,合适的弛豫时间分布点数为32～64.激发极化弛豫时间谱能够表征饱和NaCl溶液的岩石孔隙结构.结合孔隙度和弛豫时间几何平均值,能够显著提高渗透率的求取精度.  相似文献   

Precipitation of secondary Fe(III) minerals from acid mine drainage     

《Applied Geochemistry》2006,21(3):437-445

Oxidation of FeS₂ in mine waste releases ${\mathrm{SO}}_4^{2-}$, Fe(II) and H⁺, resulting in acid mine drainage (AMD). Subsequent oxidation and precipitation of Fe produces different Fe(III) phases where the mineralogical composition depends on pH and the ambient concentrations of metal ions and complexing ligands. The oxidation and precipitation of Fe in AMD has been studied under various conditions with the intent of understanding the role these processes play in the natural attenuation of metal contaminants in the AMD. The combined process of Fe oxidation and precipitation in AMD from the Kristineberg mine, northern Sweden, has been investigated with pH-stat experiments at pH 5.5 and 7 at 10 and 25 °C. The precipitates formed have been characterised in terms of mineralogy and surface area. Similar phases formed at both temperatures, while the oxidation and precipitation occurred more readily at the higher temperature and higher pH. At pH 7, mainly lepidocrocite (γ-FeOOH) was precipitated while at a lower pH of 5.5, a mixture of schwertmannite, goethite, ferrihydrite and lepidocrocite formed. The ambient Zn(II) concentration was immediately reduced to acceptable levels (according to Swedish EPA) at pH 7 whereas a 2–3 weeks ageing period was necessary to achieve the same effect at pH 5.5. The presence of natural organic matter (NOM) reduced the attenuating effect at pH 5.5 after ageing but increased it slightly at pH 7. Addition of Zn(II) at pH 8 resulted in a mixed Fe(III)–Zn(II) precipitate of unknown composition with some Zn(II) adsorbed at the surface. The Fe(III) precipitates formed are potentially useful for the natural attenuation of metal contaminants in AMD although based on these investigations, the degree of success depends upon pH and NOM concentration.  相似文献   

华南沿海地区车载风廓线雷达资料的分析与应用     

王志春  植石群  丁凌云  刘尉  黄俊 《气候与环境研究》2013,18(2):195-202

对系统风较小时车载风廓线雷达探测资料与气球探空资料进行了对比, 发现二者一致性较好, 并应用车载风廓线雷达探测资料分析了探测期间惠来海陆风的空间结构和时间演替规律。同时分析了车载风廓线雷达探 测到的“灿都”台风资料, 结果表明车载风廓线雷达对台风外围下沉气流区高空风的三维结构有较强的探测能 力, 能有效地探测到台风登陆过程中地面到高空的水平风切变和垂直气流切变过程, 有助于提高沿海地区防台风抗台风能力。  相似文献   

A model-independent method of determining energy scale and muon number in cosmic ray surface detectors     

《Astroparticle Physics》2009,30(6):355-365

  相似文献   

碳酸盐岩干酪根催化降解生烃过程及动力学研究   总被引：8，自引：0，他引：8  

赵桂瑜  李术元  刘洛夫 《地质科学》2005,40(1):47-54

以甘肃平凉地区奥陶系碳酸盐岩干酪根为对象,利用热模拟实验方法和化工催化原理,从热解生烃组成特征、生烃量及生烃动力学等方面考察了不同介质对干酪根热解生烃过程的影响。结果表明,碳酸盐岩对干酪根生烃过程具有反催化作用,随着温度的增加,反催化作用越明显。膏岩CaSO₄则表现出正催化作用,各种盐类对干酪根生烃过程影响较小。干酪根热解动力学研究表明,生烃动力学参数活化能E与视频率因子A之间不是独立变化的,它们之间存在一定的关系,即:E与lnA呈线形关系,这对于认识碳酸盐岩干酪根的化学结构及热解生烃机理具有一定的参考价值。  相似文献   

青海盐湖镁资源开发与利用研究进展   总被引：1，自引：1，他引：0       下载免费PDF全文

毕秋艳  党力  曹海莲  高莉  郭强  柴克松  鲁云花  徐世爱 《盐湖研究》2022,30(1):101-109

简要介绍了青海盐湖资源的分布、储量,重点对青海盐湖镁资源的研究开发和利用现状进行了综述,分析了其中存在的问题和关键技术瓶颈.在此基础上,对未来青海盐湖镁资源的高值化利用和研究方向进行了展望,并提出了相应的建议.  相似文献   

Temperature changes the dynamics of trace element accumulation in Solanum tuberosum L.   总被引：1，自引：0，他引：1  

Yu Li  Qiang Zhang  Runyuan Wang  Xin Gou  Heling Wang  Sheng Wang 《Climatic change》2012,112(3-4):655-672

A simulated warming manipulation was conducted to evaluate the effects of temperature increase on cadmium (Cd), lead (Pb), copper (Cu), iron (Fe) and zinc (Zn) accumulation in Solanum tuberosum L. at Dingxi, Gansu, in the semiarid northwest of China. The objective of this study was to determine if temperature increases significantly changed trace element concentrations and contents in the different ecosystem compartments by affecting soil content, soil solubility and plant capture. The results reveal that an increase in temperature will lead to a significant change in trace element concentrations and contents in Solanum tuberosum L. The strongest effects of a 3°C temperature increase are increased Cu, Zn and Fe leaf concentrations of 25, 27 and 24%, respectively; but decreases in Cd, Pb, Fe, Zn and Cu tuber concentrations of 27, 55, 41, 29 and 23%, respectively. The increasing concentrations of some trace elements in Solanum tuberosum L. leaves are related to greater retranslocation, photosynthetic capacity and growth. Warming decreases the concentrations of some trace elements in tubers, implying that tuber growth rate exceeds its metal uptake rate at higher temperatures. Indeed, it is expected that by the year 2050 the increased temperature will have induced a decrease of concentrations of Cd, Pb, Cu, Fe and Zn of 9.1, 11.5, 18.5, 16.8 and 15.8%, respectively, in tubers in the study area. In addition, the results indicate that a 1–3°C increase in temperature will improve the availability of selected trace elements and transfer potential of these elements from soil to Solanum tuberosum L.  相似文献   

坡缕石粘土对有机染料的吸附热力学研究   总被引：1，自引：0，他引：1  

郝艳玲  王远  董良宇  牛欢  陈俊峰 《岩石矿物学杂志》2009,28(6):661-664

将甘肃靖远坡缕石粘土分离提纯,通过静态吸附实验,研究了坡缕石对水中有机染料亚甲基蓝、结晶紫和苯胺蓝的吸附等温线,探讨了吸附热力学特征.实验结果显示,在实验温度范围内3种染料在坡缕石上的吸附在30 min可达平衡,吸附等温线均能较好符合Langmuir模型,饱和吸附量大小顺序为:结晶紫＞亚甲基蓝＞苯胺蓝;吸附均为吸热过程,亚甲基蓝、结晶紫和苯胺蓝的吸附焓分别为15.52、9.26和2.59 kJ/mol;吸附Gibbs函数约为-35～-30 kJ/mol,吸附熵均大于零,吸附是自发过程.  相似文献