All of the methods briefly described below are presented in detail in
a 2008 publication in Freshwater Biology,
doi:10.1111/j.1365-2427.01941.x
Sample preparation - DOC and ¹³C-DOC samples were filtered through
pre-combusted Whatman GF/F filters and the Br- samples were filtered
through 0.2 μm Gelman HT filters.
¹³C tracer generation - Tulip poplar seedlings were grown in a ¹³C-CO₂
atmosphere and dried leaves, stems, and roots were ground and
extracted in deionized water in the dark at 4°C as described in
Weigner, T. N., Kaplan, L.A., Newbold, J. D., and Ostrom, P. H. 2005.
Synthesis of ¹³C-labeled tracer for stream DOC, labeling tulip poplar
carbon with ¹³CO₂. Ecosystems 8:501-511. doi
10.1007/s10021-003-0043-1. The infusion was processed to remove
particles, stabilized through Tyndallization, and stored at 4°C prior
to use.
Dissolved organic carbon (DOC) - Measurements were made by
Pt-catalyzed persulfate oxidation in an OI 1010 analyzer.
¹³C-DOC - Analyses were performed as described in Gandhi, H., Wiegner,
T. N., Ostrom, P. H., Kaplan, L. A., and Ostrom, N. E. 2004. Isotopic
(13C) analysis of dissolved organic carbon in stream water using an
elemental analyzer coupled to a stable isotope ratio mass
spectrometer. Rapid Communication in Mass Spectrometry 18:903-906. doi
10.1002/rcm.1426. Filtered stream samples were concentrated with
rotary evaporation, acidified, lyophilized, combusted, and the
CO₂ analyzed with an elemental analyzer (EA
3000, Eurovector) interfaced to an isotope ratio mass spectrometer (GV
Instruments).
Bromide - Bromide was measured as an anion with ion chromatography
(Dionex Model 500). ¹³C-DOC tracer calculations - The ¹³C enrichment
or fractional abundance in the stream water DOC following the tracer
addition was calculated from the measured ẟ¹³C-DOC values and used in
a mixing model to estimate the fractional abundance of the for the
¹³C-DOC from the tracer and from White Clay Creek water prior to the
tracer addition.
¹³C-DOC uptake in White Clay Creek - The longitudinal loss rate curve
for the ¹³C-DOC tracer was approximated from the sum of two
first-order loss rate curves associated with labile and semi-labile
biodegradable DOC fractions. We used averaged, background-corrected,
bromide-normalized 13C-DOC plateau concentrations from the downstream
sampling sites in a nonlinear least squares analysis (PROC NLIN, SAS
Institute). From the longitudinal loss rate coefficients we calculated
uptake lengths and mass transfer coefficients for the two lability
classes.
¹³C-DOC tracer and stream water DOC lability profiling- White Clay
Creek stream water or stream water amended with the ¹³C-DOC tracer
were pumped into 8 bioreactors with empty bed contact times ranging
from 0.5 to 73.8 minutes. Influent and effluent waters from the
bioreactors were sampled and analyzed for DOC and ¹³C-DOC.
Biodegradable DOC concentrations were calculated from the differences
in concentrations between the influents and effluents to the
bioreactors.