Wastewater Engineering 727
Stabilization ponds can be classified as facultative (aerobic-anaerobic),
aerated, aerobic, and anaerobic ponds according to the dominant type
of biological activity or reactions occurring in the pond. Other classifi-
cations can be based on the types of the influent (untreated, screened,
settled effluent, or secondary (activated-sludge) effluent), the duration
of discharge (nonexistent, intermittent, and continuous), and the method
of oxygenation (photosynthesis, atmospheric surface reaeration, and
mechanical aeration). Aerated ponds (aerated lagoons) have been dis-
cussed previously.
25.1 Facultative ponds
The most common type of stabilization pond is the facultative pond. It
is also called the wastewater lagoon. Facultative ponds are usually
1.2 to 2.5 m (4 to 8 ft) in depth, with an aerobic layer overlying an anaer-
obic layer, often containing sludge deposits. The detention time is usually
5 to 30 days (US EPA, 1983b).
The ponds commonly receive no more pretreatment than screening
(few with primary effluent). It can also be used to follow trickling filters,
aerated ponds, or anaerobic ponds. They then store grit and heavy solids
in the first or primary ponds to form an anaerobic layer. The system is
a symbiotic relationship between heterotrophic bacteria and algae.
Bacteria found in an aerobic zone of a stabilization pond are prima-
rily of the same type as those found in an activated-sludge process or in
the zoogleal mass of a trickling filter. The most frequently isolated bac-
teria include Beggiatoa alba, Sphaerotilus natans, Achromobacter,
Alcaligenes, Flavobacterium, Pseudomonas, and Zoogloea spp. (Lynch
and Poole, 1979). These organisms decompose the organic materials
present in the aerobic zone into oxidized end products.
Organic matter in wastewater is decomposed by bacterial activities,
including both aerobic and anaerobic, which release phophorus, nitro-
gen, and carbon dioxide. Oxygen in the aerobic layer is supplied by sur-
face reaeration and algal photosynthesis. Algae consume nutrient and
carbon dioxide produced by bacteria and release oxygen to water. DO is
used by bacteria, thus forming a symbiotic cycle. In the pond bottom,
anaerobic breakdown of the solids in the sludge layer produces dis-
solved organics and gases such as methane, carbon dioxide, and hydro-
gen sulfide. Between the aerobic and anaerobic zones, there is a zone
called the facultative zone. Temperature is a major factor for the bio-
logical symbiotic activities.
Organic loading rates on stabilization ponds are expressed in terms
of kg BOD
5
applied per hectare of surface area per day (lb BOD/
(acre ⭈ d)), or sometimes as BOD equivalent population per unit area.
Typical organic loading rates are 22 to 67 kg BOD/(ha ⭈ d) (20 to 60 lb
BOD/(a ⭈ d)). Typical detention times range from 25 to 180 days. Typical