I. Terms and definations.
B. In case you forgot, photosynthesis converts light into high-energy
carbon bonds.
C. Because plants also use up energy through respiration, the
photosynthetic rate will not equal the amount of energy stored.
The rate of photosynthesis can be measured by analyzing the chemicals unique to either side of the photosynthesis equation (e.g., CO2, O2, or C6H12O6)
A. On Land. Place a plastic bag around a plant. Measure the change in atmospheric concentration of CO2 during the daylight hours. This will tell you NPP, as both photosynthesis and respiration are taking place. Do the same at night, which will tell you the respiration rate, as photosynthesis is not taking place. By adding these two numbers together (NPP+respiration) you will know GPP
B. In Water. Collect a bucket of water. Mix it well and measure the oxygen cencentration in the sample. Put it into two glass gars, one of which has been wrapped in aluminum foil so that no light will shine on it. Place the jars back into the water and let sit for a few hours. Measure the Oxygen levels of the two jars. The amount of Oxygen generated in the clear bottle will tell you NPP (both photosynthesis and respiration taking place), while the amount of oxygen used up in the shaded bottle will tell you Respiration. Add both to get GPP.
C. Sugar generation. Place a plant into an air-tight plastic bag. Pump radioactive CO2 into the bag, and let the plant briefly be exposed to it. Take the plant out of the bag, grind it up, and determine how much radioactive sugar has been created. This will tell you GPP directly.
III. Estimating Primary Production Efficiency.
B. GPP Efficiency is calculated by dividing GPP energy for a given area by the total sunlight energy that area is exposed to.
For example:
7.08 moles of sugar are generated via GPP per year for each square meter of Lake Mendota in Madison.
Multiplying this by 709, we calculate that 5017 kcal of sunlight is
absorbed during this process.
By putting sunlight sensors out on the
lake, we can determine that 1,188,720 kcal of sunlight falls on each square
meter of Lake Mendota during that year.
GPP Efficiency for Lake Mendota = (5017 / 1,188,720) * 100 = 0.42%
GPP Efficiency for other ecosystems:
Forests 2 - 3½%
Grasslands 1 - 2%
Crop Fields 1½%
C. NPP Efficiency is calculated by dividing NPP energy into total sunlight energy.
Because Respiration losses are greater in some systems, NPP and GPP efficiencies will not be the same. For the communities listed above, NPP Efficiency equals approxil\matley 1%, even through GPP Efficiencies were up to three times greater in some communities.
Thus, approximately 1% of sunlight is made available by plants for other organisms to consume.
On land, soil Nitrogen, water and light most often limit production
In water, Phosphorus and light most often limit production.
In aquatic systems, both too little sun, as well as too much sun, may limit produciton.
Areas with too little sun (deep in water) are photolimited
Areas with too much sun (at water surface) are photoinhibited
Maximum pproduction occurs a few meters deep into the ocean, where
sunlight levels are not as high. These areas are photosaturated.