Components of an ecosystem
-Habitat, where organisms live.
-Population, organisms of one species in an area.
-Community, populations of different species.
Biotic factors
-Living organisms within an ecosystem.
-Producers generate energy from autotrophic reactions (eg photosynthesis).
-Consumers feed on other organisms.
-Decomposers feed on waste material or dead organisms.
Abiotic factors
-Non-living components of an ecosystem.
-pH, humidity, temperature, pollutants.
-Storms and natural hazards.
-Physical features, rocks, rivers.
-Extreme intensity leads first to lack of reproduction, then growth, and finally survival.
Cyclic changes
-Repeat in a rhythm.
-Eg movement of tides, seasons.
Directional changes
-Occur in one direction.
-Last longer than the lifetime of organisms.
-Eg deposition, erosion.
Trophic level
-A level of the food chain.
-Biomass conserved decreases in higher trophic levels.
-This is because biomass is lost in respiration, metabolism, waste, and organisms dying to factors other than consumers.
-Expressed in a pyramid.
Preparation of dry mass
-Organisms put into oven at 80C until water is evaporated.
-Shows biomass of an organism.
-However, is destructive, so wet mass is measure and calculated using old dry mass data.
Ecological efficiency
-Biomass transfer between trophic levels.
-Biomass at higher level/Biomass at lower level x 100.
Gross primary productivity
-Rate at which plants convert light energy into chemical energy through photosynthesis.
-Optimum 40% of sunlight enters light reaction of photosynthesis.
-Two-thirds of glucose used in production of starch, lipids, cellulose and proteins. Rest respired.
Net primary productivity
-Energy from the sun that remains to enter the food chain from photosynthesis.
-8% in natural optimal.
Secondary productivity
-Conversion of biomass of lower trophic levels by consumers into their own biomass.
-Small amount due to excretion of waste products, and respiration.
Improving primary productivity
-Light banks to increase light harvesting.
-Irrigation and drought-resistance.
-Crop rotation increases available nutrients, stops reduction in inorganic minerals.
-Rotation coupled with nitrogen fixing plants such as peas.
-Pesticides or fungicides, or resistant strains.
Improving secondary productivity
-Harvesting animals just before adulthood, as young animals invest more energy into growth.
-Selective breeding for faster growth rates and yields.
-Constant environmental temperature, and availability of food.
Saprotrophs
-Decomposers.
-Secrete enzymes onto dead material, digesting it into small molecules.
-Absorbed into saprotroph’s body.
-Molecules are stored or respired to release energy.
Nitrogen-fixing
-Nitrogen taken from air to be used by organisms.
-Occurs in Azotobacter bacteria free living in the soil.
-Occurs in Rhizobium in root nodules of leguminous plants.
-N2 becomes NH4+.
Nitrification
-Ammonium (NH4) oxidised using Nitrosomonas bacteria into nitrite (NO2).
-Nitrite oxidised using Nitrobacter into nitrate (NO3).
-This can be absorbed by plants.
Use of nitrate in plants
-DNA production.
-Protein synthesis.
-Growth.
Ammonification
-Waste products (using a urease enzyme), dead plants, and dead animals that have eaten them are decomposed by saprotrophs.
-These release ammonium into the soil, which is then used again in nitrification.
Denitrification
-In anaerobic conditions such as waterlogged soil.
-Denitrifying bacteria convert nitrate (NO3) into nitrogen (N2) and released it into the air, where it remains inert.
Haber process
-Ammonia (NH2) converted to nitrate in factories and used to make fertilisers.
-Man-made process.
Lightning in nitrogen cycle
-Lightning hits soil.
-N2 + O2 becomes either NO2 or NO3.
-If NO2 is produced then it is converted into NO3 by Nitrobacter.
-Eventually nitrate is produced.
Carbon cycle
-CO2 in air and water enters plants through photosynthesis, with its products used in growth.
-Respiration from animals and plants releases this back into the air.
-Waste products and dead animals and plants are decomposed by saprotrophs, releasing stored carbon.
-Fossilised plants become fossil fuels, which release carbon dioxide upon combustion.
Similarities between carbon cycle and nitrogen cycle
-Gases stored in organic matter, and in atmosphere.
-Influenced by human activity.
-Transfer through death and decomposition by saprotrophs.
-Absorbed from air by processes in plants.
Differences between carbon cycle and nitrogen cycle
-No nitrifying bacteria needed in carbon cycle.
-Nitrogen gas is inert and must be converted through nitrification.
-Longer term storage in carbon (fossil fuels).
-Fewer transfers in carbon cycle.
-Different uses in plants.