C9 (the atmosphere) Flashcards
describe the atmosphere of the Earth today:
- around 78% of the atmosphere is nitrogen
- around 21% is oxygen
- small proportions of other gases, such as carbon dioxide, water vapour, and noble gases (e.g. argon)
these gases have stayed pretty constant for around 200 million years.
why can scientists not be certain about the early atmosphere?
the Earth is around 4600 million years old.
what do scientists think about the first billion years of Earth?
- intense volcanic activity. these released the gases that formed the atmosphere (i.e. water vapour)
- as the Earth cooled (couldn’t form oceans initially, as the temperatures were over 100 degrees celsius), the water vapour condensed to form the oceans
- volcanoes also released huge amounts of CO2, which is what the early Earth’s atmosphere consisted mainly of, with almost no oxygen (very much like the atmospheres of Mars and Venus today)
what gases did early volcanoes release, other than carbon dioxide and water vapour?
- nitrogen, which gradually built up in the atmosphere
- released small amounts of methane and ammonia
describe the overall early atmosphere of the Earth:
- mainly carbon dioxide
- small but increasing amounts of nitrogen
why have carbon dioxide levels decreased in the Earth’s atmosphere over time?
- the water vapour from volcanoes condensed to form oceans
- some of the carbon dioxide dissolved in the oceans to form a weak acid (carbonic acid)
- this reacted with minerals in the sea to form precipitates, which over time formed sediments of carbonate rock on the sea bed
- plants and plankton photosynthesised, taking in CO2. animals then eat the plants, taking in the carbon. these die, get covered at the bottom of the ocean, and undergo huge pressures and heat, forming fossil fuels
what was the carbon dioxide in the sea used for?
- carbon particulates and acid used to make the corals and shells of organisms such as mussels
- when these died, they formed limestone (sedimentary rock), which helps to absorb CO2 from the atmosphere
where has oxygen come from since the Earth’s early atmosphere?
- around 2.7 billion years ago, photosynthetic algae first evolved in the oceans
- photosynthesis produced oxygen (and also absorbed more carbon dioxide) which entered the atmosphere
- over the following billion years, plants evolved, increasing the amount of oxygen in the atmosphere
- at some point the level of oxygen reached the point where animals could evolve
what was the first organism to produce oxygen?
cyanobacteria
describe fossil fuels:
- formed over millions of years
- non-renewable
- contain trapped carbon (part of the carbon dioxide taken in by photosynthesis)
how is coal formed?
FOSSIL FUEL
- from the remains of ferns and trees
- over time, the plant remains are covered with sediment and compressed
- high temperature and pressure creates coal
when may coal not be formed?
if the ferns/trees die in marshy wetlands. they don’t decompose, due to a lack of oxygen/acidic conditions, both preventing bacteria from carrying out decomposition.
how is crude oil formed?
FOSSIL FUEL
from plankton (tiny plants/animals found under the sea). when they die, they settle on the sea bed (apart from in anoxic conditions, when they’re unable to decompose). over time, they’re compressed by sediment, and heat and pressure convert them to crude oil.
what is natural gas?
FOSSIL FUEL
- mainly the hydrocarbon methane
- often found near deposits of oil, as it’s formed from plankton in a similar way to crude oil
describe the small proportions of the greenhouse gases in the modern day atmosphere:
water vapour: amount varies, changes depending on temperature
carbon dioxide: around 0.04%
methane: tiny amounts
describe the greenhouse effect:
- energy from the sun travels to Earth as short wavelength radiation (e.g. ultraviolet and visible light)
- some of the short wavelength radiation simply reflects back into space, but most of it passes easily through the atmosphere, as short wavelength radiation doesn’t interact strongly with the gas molecules in the atmosphere
- the energy of the radiation is absorbed when it reaches the surface of the Earth
- the surface of the Earth now radiates energy as long wavelength radiation such as infrared
- some of these interact with the greenhouse gas molecules in the atmosphere (the energy is absorbed). this causes the temperature of the atmosphere to increase
describe the importance of the greenhouse effect:
keeps the temperature on Earth warm enough to support life.
why are the levels of carbon dioxide currently increasing?
- increasing as we burn fossil fuels (e.g. burning coal for electricity, petrol/diesel for cars, gas to heat our homes)
- rainforests are being destroyed through deforestation (usually burned) to provide land for grazing cattle, so they can’t absorb carbon dioxide
- burning the forests also produces large amounts of carbon dioxide