ch 21 : movement of elements in ecosystems Flashcards
are chemical elements reused constantly?
yes; they cycle between biologically usable and un-usable states (organic and inorganic)
what happens to energy during transformations?
it’s either gained or lost
- oxidation—gives up electrons (loses energy)
- reduction—accepts electrons (gains energy)
assimilatory processes
- inorganic –> organic
- requires energy (photosynthesis)
dissimilatory processes
- organic –> inorganic
- releases energy (respiration)
an ecosystem may be viewed as a set of _________ among which elements are cycled at various rates:
compartments
the movement of water through ecosystems and the atmosphere; including evaporation, transpiration, and precipitation.
hydrologic cycle
97% of water is found where?
in the oceans; the remaining water is in lakes, streams, rivers, wetlands, underground aquifers, and soil
the amount of ________ must balance the amount of _________ or all water would accumulate in one part of the cycle
evaporation; precipitation
what is the relationship between precipitation and evaporation on a global scale?
on a global scale, precipitation exceeds evaporation in terrestrial ecosystems; evaporation exceeds precipitation in aquatic systems.
what is the relationship between precipitation and evaporation on a global scale?
on a global scale, precipitation exceeds evaporation in terrestrial ecosystems; evaporation exceeds precipitation in aquatic systems.
what happens to excess water that falls on land?
it’s transported in runoff and groundwater into aquatic systems
what are some of the ways that humans impact the hydrologic cycle?
- creation of impervious surfaces (e.g., roofing, pavement) reduces the water that enters the soil and increases runoff.
- removing plant biomass (e.g., cutting down a forest) decreases evapotranspiration and also increases runoff.
- increased runoff causes soil erosion and flooding
- humans often use water from the ground (e.g., for irrigation) before it can be replenished.
- climate change may increase temperatures and evaporation rates, leading to increased intensity of rain and snowstorms.
what is used for respiration in oxygen-poor habitats?
carbon is used for respiration instead of oxygen
which is more effective: CO2 or CH4 (methane)?
methane is 72 times more effective as a greenhouse gas than CO2
what does the precipitation of calcium carbonate lead to?
the development of rock known as dolomite and limestone
describe the rate of carbon burial
it’s slow and is offset by rates of carbon release from limestone weathering and volcanic eruptions
what are the human impacts on the carbon cycle?
- over the past two centuries, extraction and combustion of fossil fuels (e.g., coal, oil, natural gas) has increased to meet energy demands.
- combustion of fossil fuels releases CO2 into the atmosphere.
- measurements atop Mauna Loa on the island of Hawaii indicate a 25% increase in atmospheric CO2 between 1958 and 2012.
- researchers use ice cores to measure CO2 concentrations that were in the atmosphere hundreds of thousands of years ago.
- in very cold regions (e.g., Greenland), snowfall compresses into ice over thousands of years, trapping tiny bubbles of air.
- researchers date the layers of ice in a core sample, melt the layers, and sample CO2 concentrations of the air inside trapped bubbles.
- such studies indicate that current CO2 levels in our atmosphere fluctuate greatly, but are currently 31% higher than
the maximum
concentration
during the past
400,000 years.
what does CO2 absorb? Too much of CO2 could cause the planet to what?
- CO2 is a greenhouse gas that absorbs infrared radiation.
- excessive amounts of CO2 could cause our planet to become much warmer than it has been in a very long time.
what does warming in the high latitude regions cause?
peat, which is the mixture of dead sphagnum moss and other plants, to thaw and begin decomposing
decomposing peat releases methane gas, which exacerbates the problems of excessive greenhouse gases and global warming
what is the most limiting nutrient on earth?
nitrogen
what are some other characteristics of nitrogen?
- more complex (C)
- ammonification
- organic nitrogen(proteins) ->NH3 ->NH4+ - de/nitrification
- nitrifying bacteria: NH4+ -> NO2-
- denitrification: NO2- -> N2 - nitrogen-fixing bacteria:N2 NH3 NH4+
important bacteria for nitrogen fixing
- rhizobium (in legumes, other plants) - azobacter (free-living)
important bacteria for nitrification
- nitrosomonas (soil) - nitrosococcus (ocean)