Abstract

Radioactive contaminants, such as radium, radon, and uranium isotopes are naturally present in drinking water, and gas and oil extraction like hydraulic fracturing can exasperate radionuclide leakage into groundwater. The concentration of radionuclide in drinking water is dependent upon the water source and the underlying lithology within the aquifers. In United States, the Environmental Protection Agency regulates the level of radioactivity in drinking water via the gross alpha test, which is conducted to measure the emitted alpha particles as a result of the radioactive elements’ natural decay. Radionuclides, such as radium and uranium, are known to cause bone cancer and other forms of cancer. Communities with crippling water purification infrastructure may be at a higher risk of being exposed to radionuclides, and this is a significant environmental justice concern. The radionuclide concentrations for the metropolitan or most populated city in each state in the United States and its territories (Puerto Rico, US Virgin Islands and Guam) were analyzed and correlated to the annual household income, to determine any disparities that maybe present. Lower income communities had elevated levels of radionuclides when compared to higher income communities which had lower frequency in elevated radionuclide contaminants.

Highlights

  • Radionuclides are intrinsically present in varying amounts in potable water

  • Radioactive contaminants, such as radium, radon, and uranium isotopes are naturally present in drinking water, and gas and oil extraction like hydraulic fracturing can exasperate radionuclide leakage into groundwater

  • In United States, the Environmental Protection Agency regulates the level of radioactivity in drinking water via the gross alpha test, which is conducted to measure the emitted alpha particles as a result of the radioactive elements’ natural decay

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Summary

Introduction

Radionuclides are intrinsically present in varying amounts in potable water. These radiological contaminants are released into the water source from rocks. The level of radionuclides is dependent upon the lithology of the underground structures (Agbalagba et al, 2012). Erosion and dissolution increase the concentration of radiological elements that enter the water source (Ivanovich & Harmon, 1992). Uranium-234 (234U) and Uranium-238 (238U) are the most abundant radionuclides in the Earth’s crust and in potable water. Radium-226 (226Ra), radium-228 (228Ra) and radon-222 (222Rn) are environmental isotopes which are formed as result of radioactive decay of uranium and thorium present in rock and soil (Water Quality Association, 2020)

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