Mjc. Laima et al., Distribution of adsorbed ammonium pools in two intertidal sedimentary structures, Marennes-Oleron Bay, France, MAR ECOL-PR, 182, 1999, pp. 29-35
The 1-step and multiple-step KCl extraction technique was used to evaluate
quantitatively the distribution of adsorbed NH4+ in the 0-5 cm strata of 2
intertidal muddy structures from Marennes-Oleron Bay, France. KCI extractio
n efficiency was higher in the reconstituted sediment slurries and decrease
d significantly in the presence of porewater ions, leading to underestimati
ons of the size of the pool of adsorbed, easily desorbed NH4+. Various pool
s of adsorbed NH4+ were displaced from the sediment after reaction with KCl
in multiple steps. Pools of tightly bound NH4+ were much larger in runnels
as opposed to ridges, and accounted for up to 32% (ridge) and 40% (runnel)
of the NH4+ desorbed from the sediment. These pools have important implica
tions for the calculation of the KD value, the dimensionless NH4+ distribut
ion coefficient. Differing relationships between easily desorbed NH4+ or ti
ghtly bound NH4+, on the one hand, and the sediment grain size, CaCO3 and N
content, on the other, suggest multiple origins for particulate matter in
the sediment.