Dear Ron, Dear Sir

and others,
Humic Acids (HA):
Based on UV-VIS spectra which I had recorded of several aquaria I estimate the HA content to be approx. 0.5 - 10 ppm. It can be much higher but most probably not lower. I had to make some estimates regarding molecular extinction coefficient and have used a value which very likely undeestimates the actual HA concentration. I have also taken a low molecular weight which also can lead to an underestimation.
I am also including a few cuttings:
C-Functional Group Chemistry of Humic Substances and
Their Spatial Variation in Soils
S. C. B. Myneni 1 , T. A. Warwick 2 , G. A. Martinez 3 , G. Meigs 2
1 Earth Sciences Division, Lawrence Berkeley National Laboratory, Berkeley, CA 94720, USA
2 Advanced Light Source, Lawrence Berkeley National Laboratory, Berkeley, CA 94720, USA
3 Agriculture Experiment Station, University of Puerto Rico, San Juan, PR 00936-4984, USA
Organic molecules derived from biological processes and the biochemical alteration of plant and
animal residue are common in soils and natural aquatic systems and their concentration ranges
from <1 ppm to as high as 4x10 5 ppm. Their composition varies widely with location and origin
(e.g. soil, marine), and consists of small chain molecules (e.g. acetate, citrate), organic
macromolecules (e.g. proteins), and polyfunctional humic substances (HS)1 . Of these, humic
substances exist at high concentrations, and are stable to biochemical alteration with long
lifetime.
In addition, HS can form strong complexes with both inorganic and organic
contaminants and mineral surfaces, and thus play a major role in geochemical processes 2 . At least
for a century, research has been focused on understanding the HS functional group chemistry and
the macromolecular structure - the properties of HS that control their behavior in the
environment.
The following is from an online aquariumfrontiers article by Randy:
Organics
The nature of organic molecules is certainly the most complicated aspect of seawater chemistry.
Organics comprise about 2 ppm of seawater. Of this 2 ppm, the majority is in the form of dissolved organic carbon (DOC). DOC includes all fully dissolved organic compounds and any particulates that are small enough to pass through a 0.45-micron (Ã"šÃ‚µm) glass fiber filter. Strictly speaking then, it is not all fully dissolved. Any organic particles greater than 0.45 Ã"šÃ‚µm are called particulate organic carbon (POC). The POC is about a factor of 10 lower in concentration than DOC and is composed of living and dead organisms, as well as assemblies of organic molecules.
DOC is an incredibly complicated mixture of molecules that represents billions of years of biological waste products from uncounted numbers of different organisms, combined with reactions catalyzed by light, heat, inorganic catalysts (metals), biological processes, and many other factors.
It includes carbohydrates (20 to 35 percent of the total), humic substances (10 to 30 percent of the total), amino acids and proteins (2 to 3 percent), hydrocarbons (less than 1 percent), carboxylic acids (1 percent) and steroids (trace).
There is also a great deal of uncharacterized organic material. In fact, the study of seawater organics is an active area of research. Additionally, the summation of all dissolved organics in the ocean is a pool of carbon larger than carbon dioxide in the atmosphere, so it cannot be ignored by those looking at the planetary carbon cycle. In addition to carbon, these organics contain significant amounts of oxygen, nitrogen, phosphorus, and sulfur.
It is probably also safe to say that most, if not all, closed marine systems have higher organic levels than the ocean, although hard numbers are difficult to come by. The desire to reduce these organic levels is one of the reasons for the popularity of skimmers with marine aquaria.
Anothe one:
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Humic and fulvic acids have strong affinities for most metals and therefore influence metal mobilization and bioavailability in the environment. [5,1]. Characterizing these complex multivariate interactions is fundamental to the prediction and control of metal speciation [6,1,5].
The nature of humic-metal complexation is neither understood nor agreed upon [1,6]. However, because HFAs have numerous binding sites with a continuum of binding strengths it is agreed that they can not be treated as simple, isolated molecules [7]. Because of the complexity of humic-metal interactions, their stability constants and complexation capacities depend on pH, ionic strength, metal concentration, presence of interferents, and the nature of the particular HFA [7, 8]. .........