ch. 9. aquatic ecosystems and physiology: energy flow productivity dissolved oxygen

Ch. 9.Aquatic ecosystems

and Physiology:

Energy Flow Productivity Dissolved Oxygen

Fig. 9.1. Hypothetical Trophic Structure Model. Boxes are filled with functional groups, measured as calories of energy, or moles of chemicals, biomass, or numbers.

Fig 1.14a. Energy flow model of Cedar Bog Lake, Minnesota (Lindeman 1942)

Fig 1.14b. Energy flow model of Silver Springs, Florida (Odum 1971)

PRIMARY PRODUCTIVITY: PHOTOSYNTHESIS

Fig. 9.4.

NPP = GPP – Respiration

Horne and Goldman 1994

Horne and Goldman 1994

Kalff 2002

Importance of dissolved oxygen in aquatic systems

• Affect the distribution of aerobic heterotrophic life

• Impacts the solubility of phosphorus and other nutrients

• Influences redox potential (Ch. 16) and thus the solubility of redox-sensitive materials

• May be used to estimate ecosystem productivity

Horne and Goldman 1994

Productivity may be measured in units of mgC volume-1 time-1

Because it takes two moles of O2 to fix 1 mole of C, productivity may also be measured in units of mgO2 volume-1 time-1

CO2 + H2O CH2O + O2

Ratio of moles of C to moles of oxygen = 12/32 = 0.375; i.o.w. 1 mg O2 produced = 0.375 mg C fixed

Examples of productivity measurement techniques:

Light - dark bottles

Diel cycles in oxygen levels

14C uptake

Lingeman and Ruardij, 1981

PN=PG-R

R

Kalff 2002

Kalff 2002

Kalff 2002