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波兰东北部页岩气勘探与生产产生的废物中的放射性

Radioactivity in wastes generated from shale gas exploration and production - North-Eastern Poland.

作者信息

Jodłowski Paweł, Macuda Jan, Nowak Jakub, Nguyen Dinh Chau

机构信息

AGH University of Science and Technology, Faculty of Physics and Applied Computer Science, Al. Mickiewicza 30, 30-059 Kraków, Poland.

AGH University of Science and Technology, Faculty of Drilling, Oil and Gas, Al. Mickiewicza 30, 30-059 Kraków, Poland.

出版信息

J Environ Radioact. 2017 Sep;175-176:34-38. doi: 10.1016/j.jenvrad.2017.04.006. Epub 2017 Apr 19.

DOI:10.1016/j.jenvrad.2017.04.006
PMID:28431375
Abstract

In the present study, the K-40, U-238, Ra-226, Pb-210, Ra-228 and Th-228 activity concentrations were measured in 64 samples of wastes generated from shale gas exploration in North-Eastern Poland. The measured samples consist of drill cuttings, solid phase of waste drilling muds, fracking fluids, return fracking fluids and waste proppants. The measured activity concentrations in solid samples vary in a wide range from 116 to around 1100 Bq/kg for K-40, from 14 to 393 Bq/kg for U-238, from 15 to 415 Bq/kg for Ra-226, from 12 to 391 Bq/kg for Pb-210, from a few Bq/kg to 516 Bq/kg for Ra-228 and from a few Bq/kg to 515 Bq/kg for Th-228. Excluding the waste proppants, the measured activity concentrations in solid samples oscillate around their worldwide average values in soil. In the case of the waste proppants, the activity concentrations of radionuclides from uranium and thorium decay series are significantly elevated and equal to several hundreds of Bq/kg but it is connected with the mineralogical composition of proppants. The significant enhancement of Ra-226 and Ra-228 activity concentrations after fracking process was observed in the case of return fracking fluids, but the radium isotopes content in these fluids is comparable with that in waste waters from copper and coal mines in Poland.

摘要

在本研究中,对波兰东北部页岩气勘探产生的64个废物样本中的K-40、U-238、Ra-226、Pb-210、Ra-228和Th-228活度浓度进行了测量。所测样本包括钻屑、废钻井泥浆固相、压裂液、返排压裂液和废支撑剂。固体样本中测得的活度浓度变化范围很广,K-40为116至约1100 Bq/kg,U-238为14至393 Bq/kg,Ra-226为15至415 Bq/kg,Pb-210为12至391 Bq/kg,Ra-228为几Bq/kg至516 Bq/kg,Th-228为几Bq/kg至515 Bq/kg。除废支撑剂外,固体样本中测得的活度浓度在全球土壤平均值附近波动。对于废支撑剂,铀和钍衰变系列放射性核素的活度浓度显著升高,达到数百Bq/kg,但这与支撑剂的矿物成分有关。在返排压裂液中观察到压裂过程后Ra-226和Ra-228活度浓度显著增强,但这些流体中的镭同位素含量与波兰铜矿山和煤矿废水的含量相当。

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