Soil - the foundations of sustainable agro-ecosystems Flashcards
How do we perceive soil?
Do we understand our connections to it?
The universe:
13.7 ± 0.13 billion years
Our solar system:
4.5 billion years
Virtually all elements heavier than C have originated from supernovae –exploding super-stars from before our sun existed
Soil is a major reservoir of microbial biodiversity with which humans have evolved.
The microbial world influences human wellbeing directly, and indirectly via effects on food
quality, climate and the environment.
Urban populations are so psychologically distanced from soil and food production that
they don’t recognize themselves as dependent on world’s ecosystems.
The average ‘ecological footprint’ of a human in high income countries like ours is 5-10 ha
but there are only 1.9 ha of productive land per person in the world (in 2003)
The supply of water and nutrients from soil to crops in a 15.6 million km2 area (approximately 7800 km3 of topsoil to 0.5 m) is what now largely sustains 7.2 billion humans
Soil functions: food, fibre and fuel carbon sequestration water purification climate regulation nutrient cycling habitat for organisms flood regulation
More than 70% of available freshwater is used in agriculture according to UNESCO 2001, It is estimated that it
takes 5 million litres of water to grow a hectare of maize (Pimental et al., 2004).
Soil ecosystem services-
Food production: crops and livestock Fresh water: filtration and storage Fibre: cotton, linen, wool Wood: construction, paper Fuel: wood, peat, straw, biomass Carbon and nutrient storage Climate regulation Waste detoxification and pollution control Host biodiversity and support the biodiversity of above-ground ecosystems.
Climate change effects
mean we are losing earth at an increasing rate
Food production and consumption and waste accounts for ~25-33% of global greenhouse gas emissions
Soil ecosystems are the critical foundations of human food supplies – but we are destroying this life support system!
When we lose soil, we are losing a resource that is, for practical purposes and human timespans, essentially non-renewable.
Most of the organic matter and fertility of soil is concentrated in the upper 20 cm of soil- the topsoil.
A cm of topsoil typically takes >200 years to form, yet it can be swept away in a few seasons.
How we sustainably manage agro-ecosystems now, and in the immediate future, will determine the fate of humanity- determining our quality of life and Earth’s carrying capacity for future generations.
“Each year, we lose 15 billion trees and 24 billion tonnes of fertile soil”
For every person on the planet two trees are lost and more than 3 tonnes of soil is eroded every year.
At rates of soil formation in agricultural fields it would require at least 2 ha of land per person to balance this loss- there is less than 1.9 ha of land per person in the world (Rees 2003), of which only 0.2 ha is arable land.
Estimate 35.9 Pg yr−1 of soil eroded globally in 2012 (> 4.5 tonnes per person per year)
(Compare this to the Global Land Outlook estimate of 24 bn tonnes)
There appears to have been an overall increase in global soil erosion driven by cropland expansion and human caused land use change from 2001-2012.
Large areas of global croplands and deforested regions used for grazing livestock
suffer unsustainable rates of soil erosion