Data Echoes: Sound, Evidence, and Acoustic Methods in Energy Landscapes

This paper explores an informal acoustic method developed by a group of industrial geologists working in geothermal energy landscapes in the southwest of Iceland. Through a series of ethnographic descriptions, this paper renders the work these geologists carry out in sonic terms, emphasizing how the...

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Bibliographic Details
Published in:Science, Technology, & Human Values
Main Author: Maguire, James
Other Authors: Independent Research Fund Denmark
Format: Article in Journal/Newspaper
Language:English
Published: SAGE Publications 2021
Subjects:
Online Access:http://dx.doi.org/10.1177/01622439211034575
http://journals.sagepub.com/doi/pdf/10.1177/01622439211034575
http://journals.sagepub.com/doi/full-xml/10.1177/01622439211034575
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Summary:This paper explores an informal acoustic method developed by a group of industrial geologists working in geothermal energy landscapes in the southwest of Iceland. Through a series of ethnographic descriptions, this paper renders the work these geologists carry out in sonic terms, emphasizing how they use their bodies as sonic detectors in the production of geological evidence. Sound, the paper argues, is what allows geologists to make the intractable problem of volcanic cooling doable. It does this by differentiating two forms of evidence. Primary evidence, which ends up as data in geological reports, and secondary sonic evidence, which is what establishes that this primary evidence is, in fact, evidence. The paper introduces the concept data echoes as a way to think about how sound articulates between these evidential protocols. As echo, sound works as an outside, which, while remaining external to official protocols of knowledge production, nevertheless helps to constitute distinctions that are meaningful to the production of those categories. As data echoes through the various moments of data capture, analysis, and model building, sound’s temporal form helps to predict the time frame of volcanic cooling, as it affects both the immediate energy production scenarios and the long durée of volcanic time.