Abstract

Sub-surface activity such as geologic carbon sequestration (GCS) has the potential to contaminate groundwater sources with dissolved metals originating from sub-surface brines or leaching of formation rock. Therefore, a Laser Induced Breakdown Spectroscopy (LIBS) based sensor is developed for sub-surface water quality monitoring. The sensor head is built using a low cost passively Q-switched (PQSW) laser and is fiber coupled to a pump laser and a gated spectrometer. The prototype sensor head was constructed using off the shelf components and a custom monolithic, PQSW laser and testing has verified that the fiber coupled design performs as desired. The system shows good calibration linearity for tested elements (Ca, Sr, and K), quick data collection times, and Limits of Detection (LODs) that are comparable to or better than those of table top, actively Q-switched systems. The fiber coupled design gives the ability to separate the PQSW LIBS excitation laser from the pump source and spectrometer, allowing these expensive and fragile components to remain at the surface while only the low-cost, all optical sensor head needs to be exposed to the hostile downhole environment.

Highlights

  • Geologic carbon storage (GCS) involves the injection of carbon dioxide (CO2) into deep geological formations where it will be trapped permanently[1]

  • The MC laser output is expanded by a 3X beam expander (L3 and L4) and passes through a 900 nm long wave pass (LWP) dichroic mirror (ThorLabs, DMLP900R)

  • The resulting beam is focused by a near infrared (NIR) AR coated aspheric lens (L5) with a numerical aperture (NA) of 0.55 (ThorLabs, AL1210-C)

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Summary

Introduction

Geologic carbon storage (GCS) involves the injection of carbon dioxide (CO2) into deep geological formations (e.g. saline aquifers, unmineable coal seams, and depleted oil and gas reservoirs) where it will be trapped permanently[1]. A number of technologies such as inductively couple plasma mass spectrometry (ICP-MS) and inductively coupled plasma optical emission spectroscopy (ICP-OES) exist for the measurement of water quality[6] These are mostly laboratory-based techniques and are not amendable to field measurements and analysis in a harsh-environment. Previous work in our and other laboratories has shown that underwater LIBS can successfully be used for the elemental analysis of aqueous solutions with and without a saline sample matrix These studies focus on measurements at high pressure[4,14,15,16,17,18,19,20], as well as at atmospheric pressure[21,22,23,24,25,26,27] conditions. Cooling and decay of the plasma occurs by losing energy to the shockwave, spectral emission, and to the surrounding liquid

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