Abstract
Dissolved organic matter (DOM) in the terrestrial environment may
originate from the decomposition of soil organic matter accumulated from
the degradation of vegetative residues, the release of root exudates,
the lysis of microorganisms and addition of organic wastes, such as
livestock manure, biosolids, and different composted organic residues,
or from irrigation with wastewater. The structure of DOM macromolecules
is known to vary with the following aqueous solution properties: ionic
strength, the nature of the inorganic ions, pH and dissolved organic
carbon (DOC) concentration. In aqueous solution, the DOM molecules are
amphiphilic, that is, it possesses both hydrophilic and hydrophobic
functional groups in the same molecule. This simultaneous presence, gave
rise to the conceptual surfactant like model for DOM which has been
studies in conjunction with the equilibrium surface tension at the
liquid-air interface (STeq, mN/m). Measurements of STeq of DOM solution
were reported in a relatively small number of studies for the conditions
of the aqueous solution (e.g., temperature, pH, ionic strength, the
valence of the metal ions, and DOC concentration). All studies
demonstrate the decrease in STeq with increase aqueous concentration of
the DOC. The effect of pH, however, exhibit contradictory results.
Specifically, for a given DOC concentration, the patterns reported for
STeq versus pH were different. With increasing pH values, STeq has been
reported to decrease, increase or exhibit a minimum. These contradictory
results have been attributed to the different DOC concentration examined
in each of the studies. In current study we hypothesized that the
inconsistent results of STeq vs. pH may also stem from the adsorption
kinetics of the DOM amphiphilic molecules at the liquid air interface,
which can be evaluated form dynamic surface tension measurements (STt).
The STt is approaching STeq values and commonly exhibiting an
exponential decay pattern. If for different pH values STt is not
reaching STeq, different apparent STeq vs. pH patterns can be obtain. In
this study measurement of STt and STeq as a function of pH will be
presented for DOM solutions from different origins. The analysis of the
STt curves will be demonstrated based on a short and long term diffusion
model.
Original language | English GB |
---|---|
Pages (from-to) | 11568 |
Journal | Geophysical Research Abstracts |
Volume | 16 |
State | Published - 1 May 2014 |
Event | EGU General Assembly 2014 - Vienna, Austria Duration: 27 Apr 2014 → 2 May 2014 |