Class Notes (1,100,000)
CA (620,000)
Western (60,000)
ENVSCI (100)
Lecture 3

Environmental Science 1021F/G Lecture Notes - Lecture 3: Crop Yield, Primary Production, Subsistence Agriculture


Department
Environmental Science
Course Code
ENVSCI 1021F/G
Professor
Christie Stewart
Lecture
3

This preview shows half of the first page. to view the full 3 pages of the document.
Food and Land
Ecosystem: Interrelationships between environment and living organisms; energy flow
Species: aquatic/terrestrial
Wildlife: undomesticated
-30%-40% of global cropland has been environmentally degraded
>we are using it above its sustainable yield
-Fertility of worlds soil reaching
peak that will threaten food
supplies, scientists warn
Soil: mixture of eroded rock,
organic material, nutrients, water,
air, living organisms
-potentially renewable resource,
slowly renewed, filters and holds
water, varying levels of maturity
O horizon: Organic material
provides the base
A horizon: topsoil, the most
nutrient dense horizon, where the
roots and living organisms will be.
Has humus, mostly broken down
B horizon: Fewer organic material,
trees often root here
C horizon: also known as parent
material, where soil begins to be
made.
Soil Types:
1) Deciduous soil: large O
horizon because of the
constant organic input
(shedding of leaves)
2) Coniferous forest: A horizon is
not well developed, because needles are acidic, making the soil acidic. A lot colder which
does not make it ideal for organisms breaking down the organic material.
3) Tropical forest soil: lots of rain fall, the nutrients get washed away or get taken up by
vegetation.
4) Desert Soil: rain is absent, not a lot of organic material being input, soil is nutrient poor.
5) Grassland soil: some grasslands are seasonal, they vary, the grass dies. A lot of nutrients.
You're Reading a Preview

Unlock to view full version