A. Ledin et al., MEASUREMENTS IN-SITU OF CONCENTRATION AND SIZE DISTRIBUTION OF COLLOIDAL MATTER IN DEEP GROUNDWATERS BY PHOTON-CORRELATION SPECTROSCOPY, Water research, 28(7), 1994, pp. 1539-1545
Photon correlation spectroscopy (PCS) was applied for the characteriza
tion (concentration and size distribution) of colloidal matter in a de
ep groundwater. The measurements were performed on-line and in situ at
the Aspo underground Hard Rock Laboratory, Oskarshamn, Sweden, The co
lloidal concentration in the rather saline groundwater was not above 0
.1 mg/l and probably below 0.03 mg/l, according to the field measureme
nts and with calibrations of the PCS-instrument with well-defined refe
rence colloids of alpha-Fe2O3, gamma-Al(OH)(3) and SiO2.The results cl
early demonstrated that the stability and concentration of a colloidal
-size suspended phase in an anoxic groundwater with high Fe(II) conten
t, like the one in Aspo (0.3 mg/l), is sensitive to exposure to atmosp
heric conditions during the handling of the sample. Diffusion of air i
nto the closed measuring cuvette was enough to alter the colloidal con
tent significantly within 6 h. A particle fraction with a size distrib
ution range of 170-700 nm was formed within 45 min when air was allowe
d to diffuse into the aqueous phase from the air-filled upper part of
the cuvette. The corresponding time to generate a significant colloida
l precipitate was less than 1 min (size distribution range 100-600 nm)
when a stream of air (1.5 mi) was bubbled through the water samples.
The precipitating colloidal phase was a mixture of ferric hydroxide an
d calcium carbonate in all three cases.