Fracking bad language – hydraulic fracturing and earthquake risks

Q2 Social Sciences Geoscience Communication Pub Date : 2020-08-25 DOI:10.5194/gc-2020-33
J. Roberts, C. Bond, Z. Shipton
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引用次数: 3

Abstract

Abstract. Hydraulic fracturing, or fracking, is a borehole stimulation technique used to enhance permeability in geological resource management, including the extraction of shale gas. The process of hydraulic fracturing can induce seismicity. The potential to induce seismicity is a topic of widespread interest and public concern, particularly in the UK where seismicity induced by hydraulic fracturing has halted shale gas operations and triggered moratoria. Prior to 2018, there seemed to be a disconnect between the conclusions of expert groups about the risk of adverse impacts from hydraulic-fracturing-induced seismicity and the reported level of public concern about hydraulic fracturing induced seismicity. Furthermore, a range of terminology was used to describe the induced seismicity (including tremors, earthquakes, seismic events, and micro-earthquakes) which could indicate the level of perceived risk. Using the UK as a case study, we examine the conclusions of expert-led public-facing reports on the risk (likelihood and impact) of seismicity induced by hydraulic fracturing for shale gas published between 2012 and 2018 and the terminology used in these reports. We compare these to results from studies conducted in the same time period that explored views of the UK public on hydraulic fracturing and seismicity. Furthermore, we surveyed participants at professional and public events on shale gas held throughout 2014 asking the same question that was used in a series of surveys of the UK public in the period 2012–2016, i.e. “do you associate shale gas with earthquakes?”. We asked our participants to provide the reasoning for the answer they gave. By examining the rationale provided for their answers, we find that an apparent polarisation of views amongst experts was actually the result of different interpretations of the language used to describe seismicity. Responses are confounded by the ambiguity of the language around earthquake risk, magnitude, and scale. We find that different terms are used in the survey responses to describe earthquakes, often in an attempt to express the risk (magnitude, shaking, and potential for adverse impact) presented by the earthquake, but that these terms are poorly defined and ambiguous and do not translate into everyday language usage. Such “bad language” around fracking has led to challenges in understanding, perceiving, and communicating risks around hydraulic-fracturing-induced seismicity. We call for multi-method approaches to understand the perceived risks around geoenergy resources and suggest that developing and adopting a shared language framework to describe earthquakes would alleviate miscommunication and misperceptions. Our findings are relevant to any applications that present – or are perceived to present – the risk of induced seismicity. More broadly, our work is relevant to any topics of public interest where language ambiguities muddle risk communication.
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水力压裂脏话-水力压裂和地震风险
摘要水力压裂是一种钻孔增产技术,用于提高地质资源管理中的渗透率,包括页岩气的开采。水力压裂过程会诱发地震。引起地震活动的可能性是一个广泛关注和公众关注的话题,特别是在英国,水力压裂引起的地震活动已经停止了页岩气的开采,并引发了暂停。在2018年之前,专家小组关于水力压裂诱发地震活动不利影响风险的结论与公众对水力压裂诱发地震活动的关注程度之间似乎存在脱节。此外,还使用了一系列术语来描述诱发地震活动(包括震颤、地震、地震事件和微地震),这些术语可以指示感知风险的水平。以英国为例,我们研究了2012年至2018年间发表的由专家主导的面向公众的页岩气水力压裂诱发地震活动风险(可能性和影响)报告的结论,以及这些报告中使用的术语。我们将这些结果与同一时期进行的研究结果进行了比较,这些研究探讨了英国公众对水力压裂和地震活动的看法。此外,我们对2014年举办的页岩气专业和公共活动的参与者进行了调查,并提出了与2012-2016年英国公众调查中使用的问题相同的问题,即“你是否将页岩气与地震联系起来?”我们要求我们的参与者为他们给出的答案提供理由。通过检查他们给出的答案的理由,我们发现专家之间明显的观点两极分化实际上是对用于描述地震活动性的语言的不同解释的结果。有关地震风险、震级和规模的语言含糊不清,让人们的反应感到困惑。我们发现,在调查回复中使用了不同的术语来描述地震,通常是为了表达地震带来的风险(震级、震动和潜在的不利影响),但这些术语定义不清,含糊不清,不能翻译成日常语言使用。这种关于水力压裂的“不良言论”给理解、感知和传达水力压裂诱发地震活动的风险带来了挑战。我们呼吁采用多种方法来理解围绕地球能源资源的感知风险,并建议开发和采用一种共享的语言框架来描述地震,以减轻误解和误解。我们的发现与任何存在或被认为存在诱发地震活动风险的应用有关。更广泛地说,我们的工作与任何公众感兴趣的话题有关,这些话题的语言含糊性混淆了风险沟通。
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来源期刊
Geoscience Communication
Geoscience Communication Social Sciences-Communication
CiteScore
3.30
自引率
0.00%
发文量
26
审稿时长
20 weeks
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