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LEAD Action News Volume 22 Number 4 December 2024 Page 47 of 131
al. 1991). This means that if we measured an adult who was severely exposed one month ago, we
would only be able to identify half of the exposure from our lagged measurement. This is further
complicated when we look at children’s biokinetics and blood lead turnover. Previous studies have
shown children have a blood lead half-life of less than one week, so the measurement from blood is
incredibly time sensitive (Specht, Lin et al. 2016, Specht, Weisskopf et al. 2018). This effect introduces
a great deal of uncertainty into a single measurement of blood lead, as, in any given week, the blood
lead could change by more than 50%. In order to properly assess the exposure to lead over time using
blood lead, there would need to be serial measurements taken over many weeks at the known point of
highest exposure.
Bone lead is the most valuable tool for accurately determining cumulative exposure to lead
over years to decades. When lead gets in the body, it acts similarly to calcium, as they have similar
binding properties (Rabinowitz 1991). As a consequence, lead can disrupt critical neural pathways
reliant on calcium channels, as well as produce many other ill-effects throughout the body (Bressler
and Goldstein 1991). Lead will also replace calcium in bone. Not only is lead in bone a good marker of
overall exposure, but, since it is directly related to disruption in calcium metabolism, it is a proxy for
lead’s effects in the brain and throughout the body (United States. Agency for Toxic Substances and
Disease Registry. 2007). This is what makes bone such an excellent marker of exposure. Additionally,
since bone changes slowly in the body, studies have shown that lead measured from bone is reflective
of years to decades worth of exposure due to the slow kinetic processes of bone remodeling (Nilsson,
Attewell et al. 1991, Rabinowitz 1991, Barbosa, Tanus-Santos et al. 2005). Thus, a single measurement
of bone lead reflects the lead exposure during a time period of potential exposure from an acute or
chronic source in an individual’s past (i.e., the water crisis). Thus, we can use bone lead to identify lead
exposure that was missed due to the poor temporality, high uncertainty, and unavailability of
widespread blood lead testing from years prior.
Bone lead can be measured in a variety of ways, but the most successful and least invasive
method is a tool utilizing x-ray fluorescence (XRF) (Wielopolski, Ellis et al. 1986, Hu, Milder et al.
1989, Todd, Moshier et al. 2001). In XRF, an X-ray source generates a photon beam that passes
through the sample. The photon transfers the energy and displaces an electron from atoms in the
sample. Displacement of this electron makes the sample atoms unstable and electrons jump from
outer orbitals to lower orbitals releasing fluorescence, characteristic of the element of each atom. The
fluorescence in the form of secondary X-rays is measured by a radiation spectrometer and the rate of
determination of these secondary rays gives the elemental concentration present in the sample. XRF
has been used for decades to determine the bone lead level of individuals from children to adults in a
variety of different settings (Wielopolski, Ellis et al. 1986, Bleecker, Mcneill et al. 1995, McNeill, Stokes
et al. 2000, Grashow, Spiro et al. 2013, Specht, Lin et al. 2018). Lead can be measured at multiple
energies particular to the XRF device, the K- and L-shell. K and L are reflective of the electron orbitals
in which the measurement arose. K-shell requires the use of a radioisotope source or a high energy
radiation source. L-shell can be used with either radioisotope or x-ray tube sources. Both have been
used successfully in measurement of bone lead (Wielopolski, Ellis et al. 1986, Hu, Milder et al. 1989,
Todd, Moshier et al. 2001). There have been a number of iterations of these XRF devices to gradually
make this measurement of bone lead easier through the years.
Measurement of bone lead has become much more convenient as the capabilities of the XRF
technology has improved. The first devices to measure bone lead (K-shell) utilized a radioisotope
source (cobalt-57 and cadmium-109), which made the devices themselves fairly difficult to obtain and
operate (Hu, Milder et al. 1989). The measurement systems were also incredibly large, requiring