Ch 4 : Water, Food Production Systems and Society
Hydrological cycle: system of water flows and storages that may be disputed by human activity
energy from solar radiation driven this cycle
Water budget: quantitative estimate of the amount of water in storages and flows of the water cycle
Renewable resources: atmosphere, rivers
Non-renewable resources: oceans, icecaps
Middle group: groundwater aquifers
Human impact on the water cycle:
Withdrawals: domestic use, irrigation in agriculture and industry
Discharges: by adding pollutants to water
Changing speed at which water can flow and where it flows
Diverting rivers or sections of rivers
Transfers: occur when it stays in the same state:
Flooding
Surface runoff
Stream flows and current
Transformations: when it changes state to and from water:
Evaporation: liquid to water
Condensation: water vapour to liquid
Freezing: solid snow to ice
Ocean currents: are movements of water both horizontally and vertically
have an important role in energy discharges that influence changes
Surface currents: moved by the wind
earth’s rotation deflects them and increases their circular movement
Deep water currents (thermohaline currents): influenced by the oceanic conveyor belt
difference in water density (salt and temperature)
warm water vs. cold water
movement of water (warm and cold)
Cold ocean currents run from poles to the equator, warm water currents flow from the equator to the poles
Water has higher specific heat capacity (amount of heat needed to raise the temperature of the unit of matter by 1 degree celsius)
Ocean currents and climate:
Affects location in terms of climate
Difference temperature and whether
Land close to seas and oceans has mild climate with moderate winters and cool summers
Access to an adequate supply of freshwater varies widely
Climate change may disrupt rainfall patterns and further affect thus access
Demand for freshwater increases as population, irrigation and industrialization increases
Freshwater supply may become limited
Scarcity of water resources can lead to conflict between human populations especially when resources are shared
Humans use freshwater for:
Domestic purposes used at home
Agriculture, irrigation for animals
Hydroelectric power generation
Transportation
Making boundaries between nation rivers
Sources of freshwater:
Surface freshwater
Underground aquifers (water can be extracted from surface or wells)
Freshwater conflict:
climate change distributing rainfall patterns (causing inequalities)
irrigation which leads to soil degradation
Solutions:
increase freshwater supplies by reservoirs, desalination plants rainwater and harvesting
irrigation: select drought resistant crops
Irrigation: results in soil degradation especially in dry areas
Our water supply is sufficient, however, like food, distribution is uneven
Salinization: process of naturally dissolving minerals in the top layer of the soil which makes it too salty (saline) for further agriculture
Continental shelf: extension of continents under the seas and oceans (creates shallow water)
has 50% of oceanic productivity but 15% of its area
light reaches shallow seas so producers can be photosynthesize
countries can claim, exploit, and harvest it
Zooplankton: single-celled animals that eat phytoplankton and their waste
Fishery: when fish are harvested in a certain way
90% oceans and 10% freshwater
70% of the world’s fisheries are exploited
Aquaculture: farming aquatic organisms (coastal and inland) involving interventions in the rearing process to enhance production
Impacts of fish harms: loss of habitat, pollution, spread of diseases, escaped species may survive to interbreed with wild fish, escaped species may autocomplete native species
Maximum Sustainable yield (MSY):
SY: increase in natural capital (natural income that can be exploited each year without depleting original stock)
MSY: highest amount that can be taken without permanently deleting the stock
Pollutants can be: anthropogenic or natural, point or nonpoint source, organic or inorganic, direct or indirect
Organic
pollutant: sewage, animal waste, pesticide
example: human waste, insecurities
effects: eutrophication, loss of biodiversity
Inorganic:
pollutant: nitrates and phosphates radioactive material, heavy toxic material
example: industry, nuclear power stations, fertilisers
effects: eutrophication, bioaccumulation, biomagnification
Both:
pollutant: solid domestic waste, debris, suspended solids
example: silt form construction, household garage
effects: damage controls, plastics
Freshwater pollution: agricultural runoff, sewage, solid domestic waste
Marine pollution: rivers, human pollution, pipelines
Measuring water pollution:
BOD: amount of dissolved oxygen required to breakdown organic material in a given volume of water
Indicator species: plants and animals that show something about the environment by their presence, absence, abundance
Biotic index: indirectly measures pollution by assessing the impact on species within the community according the their tolerance, diversity, and relative abundance
Eutrophication: when lakes and coastal waters receive inputs of nutrients (nitrates and phosphates) that result in an excess growth of plants and phytoplankton
The eutrophication process:
Fertiliser enters rivers/lakes
High level of phosphates, algae grows faster
More algae, more food for zooplankton or small animals that feed on them. A lack of zooplankton animals means that these are less to eat algae
Algae die and are decomposed by aerobic bacteria
Not enough oxygen is present therefore everything dies and the food chain collapses
oxygen levels fall lower, dead organic material sediments on the lake or the river bed and turbidity increases
All life is gone and sediment settles to leave a clear blue lake. This process in which bodies of water become enriched with nutrients and minerals
Biochemical oxygen demand: amount of DO required to break down organic material in a given volume of water
biological monitoring and indicator species can be used to determine levels of pollution
strengths: stationally, sensitive and representative
weaknesses: identification
Hydrological cycle: system of water flows and storages that may be disputed by human activity
energy from solar radiation driven this cycle
Water budget: quantitative estimate of the amount of water in storages and flows of the water cycle
Renewable resources: atmosphere, rivers
Non-renewable resources: oceans, icecaps
Middle group: groundwater aquifers
Human impact on the water cycle:
Withdrawals: domestic use, irrigation in agriculture and industry
Discharges: by adding pollutants to water
Changing speed at which water can flow and where it flows
Diverting rivers or sections of rivers
Transfers: occur when it stays in the same state:
Flooding
Surface runoff
Stream flows and current
Transformations: when it changes state to and from water:
Evaporation: liquid to water
Condensation: water vapour to liquid
Freezing: solid snow to ice
Ocean currents: are movements of water both horizontally and vertically
have an important role in energy discharges that influence changes
Surface currents: moved by the wind
earth’s rotation deflects them and increases their circular movement
Deep water currents (thermohaline currents): influenced by the oceanic conveyor belt
difference in water density (salt and temperature)
warm water vs. cold water
movement of water (warm and cold)
Cold ocean currents run from poles to the equator, warm water currents flow from the equator to the poles
Water has higher specific heat capacity (amount of heat needed to raise the temperature of the unit of matter by 1 degree celsius)
Ocean currents and climate:
Affects location in terms of climate
Difference temperature and whether
Land close to seas and oceans has mild climate with moderate winters and cool summers
Access to an adequate supply of freshwater varies widely
Climate change may disrupt rainfall patterns and further affect thus access
Demand for freshwater increases as population, irrigation and industrialization increases
Freshwater supply may become limited
Scarcity of water resources can lead to conflict between human populations especially when resources are shared
Humans use freshwater for:
Domestic purposes used at home
Agriculture, irrigation for animals
Hydroelectric power generation
Transportation
Making boundaries between nation rivers
Sources of freshwater:
Surface freshwater
Underground aquifers (water can be extracted from surface or wells)
Freshwater conflict:
climate change distributing rainfall patterns (causing inequalities)
irrigation which leads to soil degradation
Solutions:
increase freshwater supplies by reservoirs, desalination plants rainwater and harvesting
irrigation: select drought resistant crops
Irrigation: results in soil degradation especially in dry areas
Our water supply is sufficient, however, like food, distribution is uneven
Salinization: process of naturally dissolving minerals in the top layer of the soil which makes it too salty (saline) for further agriculture
Continental shelf: extension of continents under the seas and oceans (creates shallow water)
has 50% of oceanic productivity but 15% of its area
light reaches shallow seas so producers can be photosynthesize
countries can claim, exploit, and harvest it
Zooplankton: single-celled animals that eat phytoplankton and their waste
Fishery: when fish are harvested in a certain way
90% oceans and 10% freshwater
70% of the world’s fisheries are exploited
Aquaculture: farming aquatic organisms (coastal and inland) involving interventions in the rearing process to enhance production
Impacts of fish harms: loss of habitat, pollution, spread of diseases, escaped species may survive to interbreed with wild fish, escaped species may autocomplete native species
Maximum Sustainable yield (MSY):
SY: increase in natural capital (natural income that can be exploited each year without depleting original stock)
MSY: highest amount that can be taken without permanently deleting the stock
Pollutants can be: anthropogenic or natural, point or nonpoint source, organic or inorganic, direct or indirect
Organic
pollutant: sewage, animal waste, pesticide
example: human waste, insecurities
effects: eutrophication, loss of biodiversity
Inorganic:
pollutant: nitrates and phosphates radioactive material, heavy toxic material
example: industry, nuclear power stations, fertilisers
effects: eutrophication, bioaccumulation, biomagnification
Both:
pollutant: solid domestic waste, debris, suspended solids
example: silt form construction, household garage
effects: damage controls, plastics
Freshwater pollution: agricultural runoff, sewage, solid domestic waste
Marine pollution: rivers, human pollution, pipelines
Measuring water pollution:
BOD: amount of dissolved oxygen required to breakdown organic material in a given volume of water
Indicator species: plants and animals that show something about the environment by their presence, absence, abundance
Biotic index: indirectly measures pollution by assessing the impact on species within the community according the their tolerance, diversity, and relative abundance
Eutrophication: when lakes and coastal waters receive inputs of nutrients (nitrates and phosphates) that result in an excess growth of plants and phytoplankton
The eutrophication process:
Fertiliser enters rivers/lakes
High level of phosphates, algae grows faster
More algae, more food for zooplankton or small animals that feed on them. A lack of zooplankton animals means that these are less to eat algae
Algae die and are decomposed by aerobic bacteria
Not enough oxygen is present therefore everything dies and the food chain collapses
oxygen levels fall lower, dead organic material sediments on the lake or the river bed and turbidity increases
All life is gone and sediment settles to leave a clear blue lake. This process in which bodies of water become enriched with nutrients and minerals
Biochemical oxygen demand: amount of DO required to break down organic material in a given volume of water
biological monitoring and indicator species can be used to determine levels of pollution
strengths: stationally, sensitive and representative
weaknesses: identification