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排序方式: 共有334条查询结果,搜索用时 15 毫秒
281.
282.
2012年6月24日宁蒗5.7级地震发生前,地震活动性存在中期异常,地下流体存在中短临异常。地震活动性方面存在滇西地区5级以上地震东西迁移规律性活动、滇西地区4级以上地震成条带分布和程海断裂发生4级窗口地震等中期震兆异常。水氡、固体二氧化碳、水温和流量存在中短临前兆异常。地下流体前兆中期、短期和短临阶段都出现同步性异常。 相似文献
283.
Phenol is one of the main pollutants in phenol wastewater and has been proved non‐biodegradable. In this study, based on strongly ring‐opening capability of boron doped diamond film electrode, a highly efficient and energy‐saving method with ultra‐low carbon emission is established through a combination of electrochemical oxidation and biological degradation. On one hand, electrochemical oxidation as pretreatment can solve the critical problem that phenol wastewater is a biological recalcitrant. On the other hand, the relatively low current efficiency during the late stage of electrochemical oxidation can be solved by follow‐up biological treatment, thus reduce the energy consumption and the cost significantly. More importantly, the carboxylic acids (oxidized from phenol) can be fully used as carbon source (no additional carbon source is added) for microbial growth instead of being oxidized to carbon dioxide and water through selecting optimizing sequencing batch reactor access time, so the carbon emission is greatly reduced. The results showed that it can save about 76.5% energy consumption and about 51.2% chemical oxygen demand can be used to maintain microorganism self‐reproduction. This is significant that this combined technology not only runs highly effectively at low cost, but also reduces the emission of greenhouse gas, carbon dioxide, thus environment friendly with wide application prospects. 相似文献
284.
Horst R. Marschall Rainer Altherr Angelika Kalt Thomas Ludwig 《Contributions to Mineralogy and Petrology》2008,155(6):703-717
The boron isotopic composition of zoned tourmaline in two metasediments from the island of Syros, determined by secondary-ion
mass spectrometry (SIMS), reflects the sedimentary and metamorphic record of the rocks. Tourmaline from a silicate-bearing
marble contains small (≤20 μm) detrital cores with highly variable δ
11B values (−10.7 to +3.6‰), pointing to a heterogeneous protolith derived from multiple sources. The sedimentary B isotopic
record survived the entire metamorphic cycle with peak temperatures of ∼500°C. Prograde to peak metamorphic rims are homogeneous
and similar among all analysed grains (δ
11B ≈ +0.9‰). The varying δ
11B values of detrital cores in the siliceous marble demonstrate that in situ B isotope analysis of tourmaline by SIMS is a
potentially powerful tool for provenance studies not only in sediments but also in metasediments. A meta-tuffitic blueschist
bears abundant tourmaline with dravitic cores of detrital or authigenic origin (δ
11B ≈ −3.3‰), and prograde to peak metamorphic overgrowth zones (−1.6‰). Fe-rich rims, formed during influx of B-bearing fluids
under retrograde conditions, show strongly increasing δ
11B values (up to +7.7‰) towards the margins of the grains. The δ
11B values of metamorphic tourmaline from Syros, formed in mixed terrigenous–marine sediments, reflect the B signal blended
from these two different sources, and was probably not altered by dehydration during subduction. 相似文献
285.
以东南极罗斯岛地区的3个湖泊沉积剖面为研究对象,利用紫外-可见-近红外反射光谱仪获得了沉积物样品的光谱曲线,讨论了东南极罗斯岛湖泊沉积物的光谱特征。在沉积物化学元素分析的基础上将样品分成建模集和验证集,采用偏最小二乘法建立光谱与化学元素指标的对应关系矩阵,通过验证集预测值和测定值之间的误差参数比较,发现研究的20种元素含量均能和光谱曲线建立有效的计算关系,其中,N、C、H、Mn、Ba、P、Al、Fe、K、Se、As和Hg等元素能够达到相当精确的预测水平(预测值与测量值之间的相关系数r20.90)。本研究结果表明,利用近红外反射光谱快速分析东南极湖泊沉积物中元素含量是一种潜在有效的方法。 相似文献
286.
通过对兰坪盆地古近纪野外剖面中含盐泥岩—泥质粉砂岩—粉砂岩微量和常量元素的测定,利用Adams和Couch古盐度计算公式、Walker"相当硼"判别法及锶钡比值法定量—半定量地分析了该区古盐度特征。结果表明,古盐度在6.5‰~22.05‰之间,盐度变化明显,以半咸水沉积为主,其次为淡水沉积。沉积中心主要位于云龙县—兰坪县一带,古盐度值最高,平面上表现为从沉积中心向盆地周缘盐度逐渐降低,并与其所伴生的沉积环境表现出良好的对应关系。结合盆地沉积相、古环境及古地理特征,综合分析认为云龙县—兰坪县一带含盐系地层具有优越的钾盐成矿前景。 相似文献
287.
288.
《African Journal of Marine Science》2013,35(3):269-279
The distributional ranges of Cape anchovy Engraulis encrasicolus and Natal anchovy Stolephorus holodon presently overlap at their eastern and western extremes, respectively, off South Africa’s east coast. These species might become more strongly sympatric as a consequence of changed distributions caused by climate change, possibly leading to intensified interspecific competition for trophic and other resources. A comparative analysis of the trophodynamics of the two species, which set out to assess elements of current niche partitioning between them, was conducted through morphological, dietary and stable-isotope analyses of specimens caught off South Africa’s east coast. Cape anchovy have larger gillraker spacing, gain the majority of their dietary carbon from large (>3 000 µm total length) planktonic crustaceans and occupy a higher trophic level than Natal anchovy, which have smaller gillraker spacing and gain the majority of their dietary carbon from planktonic crustaceans of two size classes (900–1 400 µm and 2 800–3 200 µm total length). These results indicate an element of trophic partitioning between the two species that will mitigate against interspecific competition. 相似文献
289.
290.
The geochemical and isotopic signature of Quaternary alluvial sediments filling a post-orogenic basin along the Tyrrhenian coasts of Italy (Cornia Plain, Tuscany) was investigated to unravel possible interactions with geothermal fluids from the Larderello geothermal field. Two cores located in the upper (UCP) and lower (LCP) sector of the plain were sampled to depths of up to 80 m. A third core in a neighbouring area not affected by geothermal activity was also sampled (Arno plain at Pisa), and its sediment composition was used as reference. The Cornia sediments (fraction < 65 μm) show high B, Cs and Sb concentrations related to a peculiar chemical enrichment of the clay fraction. They also show remarkable enrichments in As (up to 1000 μg g− 1) reflecting a contribution from local ore deposits.87Sr/86Sr ratios, ranging from 0.71022 to 0.71698, reveal the nature of the weathered mother rocks of the alluvial sediments, whereas the boron isotopic composition, varying from − 20‰ to − 10‰, suggests an interaction between the clay fraction and boron-rich fluids at temperatures greater than 50 °C. This implies that hydrothermal fluids widely circulated within the Cornia basin in the past, ultimately leading to the geochemical anomalies currently recorded in local sediments.Although natural (geogenic) in origin, these anomalies cause severe problems to the regional water management (groundwater exploitation) through leaching of trace elements into circulating groundwater, a phenomenon which has to be carefully studied and monitored. 相似文献