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Heavy metals distribution in fly ash from gangue power plant 总被引:1,自引:0,他引:1
To make assessment on its environmental security, fly ash samples were collected from the gangue power plant. Total content of heavy metals in sieved fly ash were analytically determined. We also carried out Tessier extractive experiments to check the chemical species of heavy metals. Experiment results show that the content of Cu, Zn, Pb and Cd ascend when particle size is smaller. Cu, Zn, Pb and Cd obviously enrich in particulate fly ash. The chemical species of heavy metal distribution ranking sequence generally is residual〉organic combinative〉Fe-Mn oxide combinative〉carbonate combinative〉ion-exchangeable. Lead's amiable-move species were high in proportion, amounted to 35%. Total content of Cadmium is at low level, but its ion-exchangeable species is relatively high in proportion. Nickel and zinc is mainly distributed in residue. Cu is mainly distributed in residue and organic combinative form. The content of manganese is relatively high in fly ash, and the carbonate combinative iron-manganese oxide combinative species are main chemical form. Cr is mainly distributed in residue, and its other chemical species are at low level. Compared with the soil background value of study area and Shandong Province, the content of Cu, Ni, Zn, Mn and Cr in fly ash of gangue power plant is lower. While contents of Pb and Cd were higher than background value, and amiable-move species is relatively high in proportion. They are more apt to cause heavy metal pollution. 相似文献
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胶莱盆地白垩系莱阳组泥页岩发育,且发现油气显示。通过对胶莱盆地莱阳凹陷莱阳组野外观测和室内分析,系统研究莱阳组泥页岩有机地球化学特征。胶莱盆地莱阳组烃源岩主要分布于水南段及逍仙庄段,烃源岩有机质丰度相对较高,但变化范围较大,校正TOC含量为0.22%~3.43%;干酪根类型包括Ⅱ1、Ⅱ2和Ⅲ 型,以Ⅱ1和Ⅱ2为主,腐泥组含量40%~82%,镜质组3%~33%,惰质组10%~45%,不含壳质组组分;镜质体反射率0.50%~2.22%,成熟度相对较高。通过对暗色泥页岩厚度、有机质丰度、有机质类型、镜质体反射率等特征分析,认为莱阳凹陷莱阳组水南段为页岩气有利层段。 相似文献
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淄博煤田煤系共生高岭石粘土岩地质特征 总被引:1,自引:0,他引:1
根据现场调查和钻孔资料,采用肉眼及偏光显微镜观察、X-射线衍射分析、岩石化学成分分析等方法,研究了淄博煤田石耐烦炭二叠系共生粘土岩分布特征、矿物学、岩石学特征,划分出不同类型的高岭石土岩,并对其成因进行了探讨,结果认为,7煤高岭石粘土岩来矸质量好,价值大,其特征与国外文献中提到的“Tonstein”类似,为中酸性火山灰蚀变而成,伊利石化高岭石粘土岩的发现与研究具有较高应用价值,且具有一定的理论意义。 相似文献
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根据单井岩性、沉积构造、测井以及连井剖面,对东部凹陷南段沙三上亚段进行了沉积环境和聚煤规律分析,认为:沉积环境主要为冲积扇、曲流河、辫状河、三角洲、洪泛平原、滨浅湖以及半深湖。研究发现,研究区沙三上亚段聚煤环境类型多样,目前已发现8个聚煤区:缓坡带的桃园三角洲聚煤区、黄金带辫状河聚煤区、热河台辫状河聚煤区、桃园废弃河道聚煤区、于楼废弃河道聚煤区、热河台废弃河道聚煤区,中间洼陷带的荣兴屯聚煤区、小龙湾聚煤区,聚煤区沿低洼地带呈长轴展布。煤层主要发育于辫状河泛滥平原、曲流河废弃河道、三角洲平原以及滨湖沼泽环境中,其中,辫状河泛滥平原、三角洲平原以及滨湖沼泽环境形成的煤层分布范围较广,为煤型气有利勘探区。 相似文献
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