Fermentation is the metabolic process by which microorganisms such as bacteria yeast or fungi, convert sugars and other organic compounds into various products, typically in absence of oxygen.
Yeast will always choose to anaerobically respirate even if oxygen is available
Carbon dioxide produced by the yeast during respiration are trapped in small air pockets in the dough, causing the dough to rise (increase in volume)
Yeast is killed by high temperatures when baking to ensure there is no further respiration by the yeast.
The yeast uses the sugar to respire excreting carbon dioxide and alcohol which causes the dough to rise.
To make bread yeast, sugar and flour are left in a warm place
Bread making: The alcohol evaporates during the baking process and the warmth increases the reaction rate.
Beer making: Yeast and sugar is left in a warm place.
Warm places causes increase in RoR
Beer making: The yeast uses the sugar to respire excreting carbon dioxide and alcohol which adds bubbles to the beer.
Cheese making: A starter culture of bacteria is added to warm milk. Curds are produced that are solid which are separated away from the whey (the remaining liquid). Bacteria and fungi are added to the curds to add different flavours of cheese as it matures.
Yoghurt making: A starter culture of bacteria is added to warm milk. The lactose in the milk is fermented by the bacteria to make lactic acid. The milk becomes a more viscous liquid in the process.
The gut microbiome is a complex community of microorganisms
(bacteria, viruses, fungi, and other microorganisms.
Gut bacteria reside in the gastrointestinal tract, primarily the colon.
Gut bacteria contribute to -
Digestion and Nutrient absorption
Immune system support
Metabolism regulation
Production of vitamins and short chain fatty acids
Mood and brain health
Fermentation
Lactobacillus acidophilus - found in yoghurts
Decomposers are organisms that feeds on and breaks down dead plant or animal matter - making organic nutrients available to the ecosystem
Some bacteria and fungi are decomposers
Methane create electricity
Digested sludge compost
Saprophytic bacteria break down dead organic matter
Compose heaps designed to provide optimum conditions for saprophytic bacteria.
Compose heaps: Should be watered - so they don't dry out, reducing risk of fire.
Compost heaps should be aerated by frequent turning - need oxygen to prevent anaerobic respiration
Lime can be added if the pH is too acidic in a compost heap to prevent anaerobic respiration
Compost heaps should be placed directly atop of the soil so worms can enter to consume plant material and derate heap.
The nitrogen cycle is the process by which nitrogen is recycled in the environment.
Neither plants nor animals can absorb nitrogen from the air: There 2 ways that can be talked out in the air into something easier to absorb
Nitrogen Fixing bacteria: Found in "free-living" in soil and also in the root nodules of legumes. They take nitrogen gas and change it into nitrates in the soil.
Lightning can fix nitrogen gas by splitting bond between two atoms and turning them into nitrous oxides (N2O and NO2) that dissolve in rain water and leach into the soil.
Plants absorb nitrate in soil and use nitrogen to make protein
Animals eat plants and get nitrogen they need from the proteins in the plant or animal
Waste (Urine and Faeces) from animals sends Nitrogen compounds as ammonium compounds into soil
Dead animals and plants decay and all the protein within them is broken down into ammonium compounds and released into the soil
Plant's can't absorb ammonium compounds - Nitrifying bacteria convert ammonium compounds into nitrates to be absorbed by plants to start cycle again.
Denitrifying bacteria is found in poorly aerated soil. - farmers prevent this by ploughing and turning soil.
Ammonification is when decomposers (fungi and bacteria) break down organic matter to convert Nitrogen compounds into ammonium compounds.
Carbon is taken out of the atmosphere in the form of CO2 by plants to be used by photosynthesis.
Carbon is also passed to animals (and microorganisms) by feeding
Carbon is returned to atmosphere by respiration
Decomposing microorganisms from decomposers (bacteria and fungi) release carbon dioxide back into the atmosphere
Carbon sequestration: Certain microbes contribute - helping stablise and store organic carbon in the soil, reducing amount of carbon released in atmosphere.