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The chemistry, mineralogy, and rates of transport of sediments in the ...

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4<br />

nitric/hydr<strong>of</strong>luoric acid mixture (5 :8 volumes respectively <strong>of</strong> concentrated<br />

acids) us<strong>in</strong>g high-purity acids (Aristar) for 48 hours at 140-145°C . After<br />

cool<strong>in</strong>g to room temperature, 4 grams <strong>of</strong> recrystallized reagent grade boric<br />

acid were added, <strong>the</strong> pH was adjusted to 4 .0 with ammonia, <strong>and</strong> <strong>the</strong> digest<br />

was <strong>the</strong>n transferred quantitatively to a 125 ml separatory funnel . <strong>The</strong> heavy<br />

metals were <strong>the</strong>n complexed with ammonium pyrollid<strong>in</strong>e dithicarbamate (AFDC)<br />

(2 ml <strong>of</strong> 2% solution) <strong>and</strong> extracted 3-4 times with 30 ml <strong>of</strong> carbon tetrachloride .<br />

<strong>The</strong> extract was collected <strong>in</strong> a 100 ml volumetric flask, <strong>and</strong> <strong>the</strong> solvent was<br />

<strong>the</strong>n removed from <strong>the</strong> extract with a Buchi Rotavapor evaporator . For this<br />

purpose <strong>the</strong> volumetric flask was attached directly to <strong>the</strong> evaporator via a<br />

special adaptor . Removal <strong>of</strong> solvent was carried out at relatively low temperature<br />

(50-55°C) to prevent loss <strong>of</strong> metals <strong>in</strong> <strong>the</strong> process . <strong>The</strong> residue <strong>in</strong> <strong>the</strong><br />

flask was <strong>the</strong>n oxidized with 5-ml <strong>of</strong> concentrated high-purity (Aristar) nitric<br />

acid, <strong>and</strong> <strong>the</strong> solution was made up to volume with triply distilled (twice <strong>in</strong><br />

quartz) water . <strong>The</strong> heavy metals <strong>in</strong> this aqueous matrix were <strong>the</strong>n analyzed for<br />

Cu <strong>and</strong> Zn by flameless atomic absorption, us<strong>in</strong>g a heated graphite tube atomizer,<br />

70 HGA Perk<strong>in</strong> Elmer, <strong>and</strong> a 403 Perk<strong>in</strong> Elik , Atomic Absorption Spectrophotometer<br />

. Precision, accuracy <strong>and</strong> some operational parameters are given <strong>in</strong><br />

Wagemann (1975) .<br />

<strong>The</strong> elements Si, Al <strong>and</strong> Ca were determ<strong>in</strong>ed simultaneously on a multichannel<br />

ARL X-ray spectrometer (University <strong>of</strong> Manitoba, us<strong>in</strong>g <strong>the</strong> method <strong>of</strong><br />

Wilson et al ., 1965) . This method consists essentially <strong>of</strong> fus<strong>in</strong>g <strong>the</strong> sample<br />

with lithium tetraborate at 1100°C, <strong>the</strong>n gr<strong>in</strong>d<strong>in</strong>g <strong>the</strong> fused bead with <strong>the</strong><br />

appropriate quantities <strong>of</strong> lanthanum oxide <strong>and</strong> boric acid <strong>and</strong> press<strong>in</strong>g <strong>the</strong><br />

mixture <strong>in</strong>to discs appropriate for analysis .<br />

Cation exchange capacity <strong>and</strong> ammonium acetate-extractible cations were<br />

determ<strong>in</strong>ed on Mackenzie Delta channel <strong>sediments</strong> accord<strong>in</strong>g to methods 5A1 <strong>and</strong><br />

3A2a from U . S . Dept . Agriculture (1967) . <strong>The</strong>se <strong>sediments</strong> were also extracted<br />

with HC1 to determ<strong>in</strong>e acid- .labile elements . Oven-dried (110 °C) sediment<br />

(15-25 g) was shaken with 100 ml <strong>of</strong> 1N NH40Ac <strong>and</strong> 1N HC1 for 8 hrs . <strong>The</strong><br />

solution was <strong>the</strong>n filtered through Whatman GF/C filters <strong>and</strong> analyzed for Ca,<br />

Mg, Na, K, Fe <strong>and</strong> Hn by atomic absorption spectrophotometry accord<strong>in</strong>g . t o<br />

Sta<strong>in</strong>ton et al . (1974) .<br />

X-ray diffraction, m<strong>in</strong>eral identifications <strong>and</strong> sediment particle size<br />

determ<strong>in</strong>ations were done by methods given <strong>in</strong> Brunskill et al . (1973,<br />

Appendix VII) .<br />

Data Analysis<br />

Instantaneous concentrations <strong>of</strong> suspended, sediment or particulate nutrients<br />

were obta<strong>in</strong>ed by direct measurement or analysis . Instantaneous discharge<br />

figures were generally taken from Water Survey <strong>of</strong> Canada (Davies, 1973 ; 1974) .<br />

Summations <strong>of</strong> total monthly discharges, computed from <strong>the</strong> mean discharge for<br />

each month, yielded annual discharge. Monthly <strong>rates</strong> <strong>of</strong> <strong>transport</strong> <strong>of</strong> suspended<br />

sediment <strong>and</strong> particulate nutrients were calculated from <strong>the</strong> product<br />

<strong>of</strong> <strong>the</strong> mean concentration dur<strong>in</strong>g <strong>the</strong> month <strong>and</strong> <strong>the</strong> total monthly discharge .

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