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71.
江苏省溧水县土壤环境污染预警预测方法探讨 总被引:5,自引:0,他引:5
介绍了溧县土壤环境质量的现状。溧水县主要有黄砂土、栗色土、岗黄土、黄岗土、马肝土、板浆白土、青泥条、青泥土等8种土壤类型。通过地球化学调查和对溧水县土壤的系统采样,获得了反映土壤质量的地球化学数据。通过对土壤中污染物富集历史的研究,揭示了土壤污染物的演化趋势。通过寻找零污染的历史时间结合现代土壤地球化学调查数据,建立了土壤重金属污染预警预测的数学模型。提出了影响土壤质量的关键因子和土壤污染的影响因素,得出了工业是影响土壤质量的主要因子,土壤污染在不断加速的结论。 相似文献
72.
山旺盆地的成因及其地质意义 总被引:3,自引:0,他引:3
前人一般认为山旺盆地是一个深度不大的封闭性淡水剥蚀盆地。笔者认为它是一个火山口成因的封闭—半封闭盆地。盆地的发展经历了3个发展阶段:早期为火山喷发作用形成火山口,并造成火山碎屑物堆积:中期堆积了较厚层的沉积物,主要为粘土质岩石,如硅藻质页岩、泥岩,此外,还有少量的砂岩、砾岩;晚期为玄武岩充填,致使整个盆地完全封闭。在盆地发展过程中,早期为封闭环境,中、晚期为半封闭环境。火山碎屑物的再堆积和分解对于生物死亡和埋藏可能具有重要的意义;该区第三纪中心式火山作用非常强烈,通过详细的区域地质调查,有可能找到更多的化石产地和硅藻土矿。 相似文献
73.
灰岩碳氧同位素特征与隐伏花岗岩的关系——以栗木水溪庙矿区为例 总被引:1,自引:0,他引:1
对栗木水溪庙矿区泥盆系上统融县组灰岩的碳氧同位素进行了研究,该地区灰岩的碳氧同位素组成可提供隐伏花岗岩隆起及其相关流体的重要信息。受隐伏花岗岩侵入驱动的流体与上覆融县组灰岩发生反应的温度在110℃左右,流体的初始同位素组成为δ18OSMOW=-3‰,δ13CPDB≤-7‰,反应的水岩比值(w/r)可能小于5。这种岩浆水与大气降水的混合流体与围岩之间的水岩反应使得地表灰岩的δ18O和δ13C值降低,产生负异常。研究表明,围岩的δ18O值降低受反应的水岩比值和温度控制;δ13C值降低主要与反应的水岩比值有关。反应的温度越高,w/r值越大,灰岩的碳氧同位素负异常越明显。因此,水溪庙矿区地表出露的碳酸盐地层中的碳氧同位素变化可在地球化学勘查中用于指示下伏花岗岩岩脊的隐伏位置。 相似文献
74.
K. Yang J. F. Huntington J. W. Boardman P. Mason 《Australian Journal of Earth Sciences》2013,60(6):915-922
Hydrothermal alteration mapping with spaceborne hyperspectral data was simulated in the Comstock mining district, Nevada in order to evaluate the mineral mapping capabilities of the proposed Australian Resource Information and Environment Satellite (ARIES‐1). As a result, a suite of hydrothermal alteration minerals, including kaolinite, dickite, illite, chlorite, alunite and carbonate was identified from the simulated data in the 0.4–2.5 μm wavelength region and their areal abundance variations mapped accordingly. The recognised alteration zoning shows a major change in alteration assemblages across the Comstock and Silver City Faults, and a gradual variation from north to south along the faults. In the bleached Miocene volcanic rocks, dickite, kaolinite, illite and alunite were recognised. Coexistence of dickite of relatively high temperature, high‐crystallinity kaolinite of medium temperature and low‐crystallinity kaolinite of low temperature suggests supergene processes overprinting earlier hypogene alteration. The bleached rocks probably represent hydrothermal alteration in the fluid up‐flow zones in the central and shallower parts of the hydrothermal system. Illite in the bleached zones is characterised by relatively short AI–OH band wavelengths (2190–2200 nm), indicating no or very low Fe and/or Mg contents. Fault‐controlled propylitic alteration is mapped in the central part of the district mainly in the footwall of the Comstock Fault. The associated illite is characterised mainly by medium AI–OH band wavelengths (2200–2208 nm). This propylitic alteration may be contemporaneous with Au–Ag mineralisation. Additional and more extensive propylitic zones, containing illite with long AI–OH band wavelengths (2204–2216 nm), were mapped in the southern part of the district. These zones resulted from either a pre‐mineralisation propylitic alteration, or the peripheral hydrothermal alteration in the fluid down‐flow zones of the Miocene hydrothermal system. 相似文献
75.
The broadband diffuse radiation method is improved to retrieve the aerosol refractive index imaginary part (AIP) and broadband (400-1000 nm mean) single scattering albedo (SSA). In this method, four sets of SSA selection criteria are proposed for quality control. The method is used to retrieve AIP, SSA and absorptive optical thickness (AbOT) from routine hourly-exposed pyrheliometer and paranometer measurements over 11 sites (meteorological observatories) in China during 1998-2003. Apart from one suburban site (Ejin Qi), the other urban sites are all located around big or medium cities. As shown in the retrieval results, annual mean SSA during 1998-2003 changes from 0.941 (Wuhan) to 0.849 (Lanzhou), and AIP from 0.0054 to 0.0203. The 11-site average annual mean SSA and AIP are 0.898 and 0.0119, respectively. SSA during winter is smaller for most sites. There is an evidently positive correlation between SSA and aerosol optical thickness (AOT) for all sites. There is also a positive correlation between SSA and relative humidity for most sites, but a negative correlation for a few sites, such as Kashi and ǚrǚmqi in Northwest China. 相似文献
76.
During the period between 18 August and 22 September 2006, an ultraviolet
photometric O3 analyzer, a NO-NO2-NOx chemiluminescence
analyzer, and a quartz micro-oscillating-scale particle concentration
analyzer were simultaneously used for monitoring at three different heights
each at Beijing (325-m tower) and Tianjin (255-m tower). These towers belong
to the Institute of Atmospheric Physics (IAP) of the Chinese Academy of
Sciences (CAS) and to the Tianjin Municipal Meteorological Bureau,
respectively. These measurements were used to continuously measure the
atmospheric O3 and NOx volume-by-volume concentrations and the
PM2.5 mass concentration within a vertical gradient. When combined with
meteorological data and information on the variation of vertical
characteristics of the various atmospheric pollutants in the two cities,
analysis shows that these two cities were seriously polluted by both
PM2.5 and O3 during summer and autumn. The highest daily-average
concentrations of PM2.5 near the ground in Beijing and Tianjin reached
183 μg m-3 and 165 μg m-3, respectively, while the O3 concentrations reached 52 ppb and 77 ppb, and NOx concentrations
reached 48 ppb and 62 ppb for these two cities, respectively. The variations
in the daily-average concentrations of PM2.5 between Beijing and
Tianjin were demonstrated to be consistent over time. The concentrations of
PM2.5 measured in Beijing were found to be higher than those in
Tianjin. However, the overall O3 concentrations near the ground in
Tianjin were higher than in Beijing. NOx concentrations in Tianjin were
consistently lower than in Beijing. It was also found that PM2.5
pollution in Beijings atmosphere may also be affected by the pollutants
originating in and delivered from Tianjin, and that Ti 相似文献
77.
78.
本文研究时间序列的变点问题。所给出的统计方法可用来推断一个时间序列是否存在变点,存在几个变点以及变点在什么位置。这种统计推断方法可用于气候阶段的划分。 相似文献
79.
A two-layer primitive equation model is developed in this paper. The capabilities of this model aretested by the use of multiyearly averaged January and July sea surface level pressure fields and windfields which can be diagnosed from the pressure fields. The results show that the ocean surface currentsand undercurrents in the second layer driven by the sea surface wind and the sea surface pressure areclose to the observation. The results are also compared with that of the IAP OGCM and the OSUOGCM. 相似文献
80.