Potential hazards associated with trace elements pertain to their accumulation in soils which may (1) lead to a plant toxicity condition or (2) result in increased uptake of metals into the food chain. Ten elements are of primary concern are arsenic, boron, cadmium, copper, mercury, molybdenum, nickel, lead, selenium, and zinc. Of these cadmium has the most dangerous long-term effects on human health. Many of these are amplified in the food chain. All logical pathways by which pollutants in biosolids could reach various biological species in the environment were included in USEPA's models that were examined in preparing the 40 CFR Part 503.
Constituent Concentrations in Wastes |
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| Waste Code | Regulated Constituent | Wastewater Concentration (mg/L) | Nonwastewaters Concentration (mg/L) |
| D004 | Arsenic | 5.0 | 30 |
| D005 | Barium | 100 | NA |
| D006 | Cadmium | 1.0 | NA |
| D007 | Chromium (Total) | 5.0 | NA |
| D008 | Lead | 5.0 | NA |
| D009 | Mercury | 0.20 | NA |
| D010 | Selenium | 1.0 | NA |
| D011 | Silver | 5.0 | NA |
Adverse effects
When an plant reaches the threshold concentration limit for a particular element, the growth and the metabolism of that plant is severely effected. Even essential elements for plant growth have a threshold limit concentration limit. Applying sewage sludge may lead to higher yields by supplying essential nutrients and improving soil properties. This practice is also one of the more common methods for concentrating trace elements in the soils.
Cadmium, Copper, Nickel and Zinc are four trace
elements in sludge that pose a hazard to plants, animals and
humans. Cadmium has caused adverse health effects in humans who
have eaten food grown on Cd rich soils. Copper, Nickel and Zinc
were shown to accumulate to toxic levels in plants.
Any element can have adverse health effects if the concentrations
are high enough. The following table shows the species groups
that are at risk from trace and toxic elements. (Hagedorn, 96)
Element |
Human |
Animals |
Aquatic Systems |
Birds |
Plants |
| Cd | yes | yes | yes | yes | yes |
| As, Pb, Hg, Cr, Se | yes | yes | yes | yes | no |
| Cu, Ni, Zn | no | no | yes | no | yes |
| Mo, F, Co | no | yes | no | no | no |
| B | no | no | no | no | yes |
This next table shows the biological functions and toxicity of
important trace elements. (Hagedorn, 96)
Element |
Biological Function |
Phototoxicity ug/g conc in leaf tissue |
Mammalian Toxicity |
Soil Range mg/Kg |
| Al | activates succinic dehydrogenase | moderate(50-200) | low | 10,000 to 300,000 |
| As | none in animals phospholipid in algae and fungi |
moderate to high (5-20) |
high | 3.6 to 8.8 |
| Cd | none known | moderate to high (5-30) |
high | 0.06 to 1.1 |
| Cr | Sugar metabolism in mamals | moderate to high (5-30) |
high | 20 to 85 |
| Cu | essential to all organisms
-redox enzymes -oxygen transport pigments |
moderate to high (20-100) |
moderate | 14 to 29 |
| Fe | essential to all organisms
-cofactior in many enzymes, proteins |
low (>1000) | low | 50 to 1000 |
| Hg | none known | high (1-3) | high | 0.04 to 0.28 |
| Mn | essential to all organisms
-splits water in photosynthesis |
low to moderate (300-500) |
moderate | 260 to 840 |
| Mo | essential to almost
all organisms -cofactor in Nitrogen fixation |
moderate(10-50) | moderate | 0.35 to 5.8 |
| Ni | essential to plants | moderate to high (10-100) |
moderate | 13 to 30 |
| Pb | none known | moderate(10-100) | high | 17 to 26 |
| Se | Essential to mammals and some plants | moderate to high (5-30) |
high | .019 to 1.05 |
| Zn | essential to all organisms | low to moderate (100-400) |
low to moderate | 34 to 84 |
Mobility in Soils
Small amounts of Cd, Cu, Ni, and Zn occur in soil solution because they are tightly held by the soil surfaces. The largest threat to surface waters is from soil erosion rather than leaching of these metals to the ground water. Soils with large amount of hydrous oxides and phyllosilicates are best to adsorb these metals and reduce the chance of leachate problems.
The metals Cd and Hg are adsorbed less intensely and pose a larger threat to movement and availiblity. Cd is a slightly soluble metal that behaves similarly to Ca in the soil solution. Above a pH of 7, Cd will precipitate which will limit solubility and mobility. Mercury has a different fate when released into a soil body. Mercury volitalizes and is released as a gas when in a soil body. This reaction is greatly increased when saturated soil conditions exsist. The toxic substance dimethyl mercury is quite toxic and can be found in reduced aquatic environments.
Fate of trace elements in soils.
There are four main processes for the solution phase concentration of trace elements:
Ionic exchange
Layer silicates in the soils provide permanent charges and ph dependent charges which retain trace metal cations by nonspecific electrostatic forces. These elements compete with Ca and Mg for the available exchange sites. Trace elements are retained to higher concentrations when in lower ph systems. At a higher ph, metal hydrolysis is more prevalent and is the domimant reaction. Cd, Cu, Cr,Hg,Pb Ni and Zn are the main trace elements that are of greatest concern on a waste treatment facility.
Precipitation reactions
When an element undergoes a precipitaition reaction, a certain
sequence happens in the process as the concentration of the
element in solution increases.
The major classes of precipitates found in soils are silicates oxides ,carbonates, phosphates and sulfates. These precipitates form salts in the system which are not beneficial to the soil system or the waste treatment system. Precipitate reactions are completely reversible and still have some dissolution properties even in stable solid phases.
Sorption to Hydrous Oxide surfaces
This process involves the altering of the surface charge
using adsorbtion or chemisorption. Trace elements in the form of
cations and anions will form short directional bonds with oxide
surfaces.
The following table shows cations and anions relative strengths
in forming bonds with soil particles. (Hagedorn, 96)
Cation's relative bonding strengths
No bond |
Weak |
Strong |
| Na+ | Mg+ | H+, Ag+, Al+3 |
| K+ | Ca+2 | Cd+2, Co+2, Cr+3 |
| NH4+ | Mn+2 | Cu+, Cu+2, Fe+2 |
| Cs+ | Sr+2 | Fe+3, Hg+, Hg+2 |
Anion's relative strengths
No bond |
Weak to Moderate |
Strong |
| NO3- | SO4-2 | OH- |
| Cl- | CrO4-2 | HPO4- |
| SeO4-2 | AsO2- | |
| MoO4-2 |
Complex formation with soil organic matter
Soil organic matter has many functional groups
contained in it that can serve as exchange sites.
Most of the compounds in question are functional groups
high in oxygen. Groups found in soil organic matter and
react with trace elements will most likely contain either COOH
groups or OH groups. These functional groups help drive the
complex reactions in the organic matter. Trace metal
compounds are tied up by the highly reactive oxygen groups and
hold the metals in place.