Chapter 4 Flashcards
Sedimentary Cycle
-most matter in lithosphere
Gaseous Cycle
most matter in atmosphere
6 nutrients on earth (97% of organic mass)
C O H P N S
Residence Time
how fast something moves through a system or stays in a particular region in space
Gaseous phase
speeds up a cycle- gas molecules move quickly
Hydrological Cycle
water plays a major role in mobilization and transport of materials
Phosphorus
- macronutrient needed in great amounts
- essential for metabolism
- relatively rare and thus a limiting nutrient
- not in atmosphere (ONLY ONE)
- plants good at storing
- can be stored in terrestrial biosphere for 100 years
- limiting macronutrient
Human impact on P cycle
- mining for fertilizer and detergent
- excess runoff into aquatic ecosystems
- water pollution
- biomass removal (accelerated erosion into streams, cut down trees=remove P)
- large [ organisms ]= lots of phosphates rich waste materials
- remove from ocean via fishing
Ocean Dead Zone
near major cities from sewage running into ocean
Sulphur
- building component of proteins
- atmospheric component
- not limiting
- can have too much sulphur sometimes
- plants need chemoautotrophs to transform S from lithosphere (sydney tar ponds)
- naturally released from volcano
- wetlands have lots of sulphur
Human Intervention on S cycle
- Burning coal that contains sulphur
2. smelting metal ores that contain sulphates
Montreal Protocol
required scrubbers on smoke stacks to get rid of sulphur
- 99% of SO2 and 33% of S in atmosphere is due to humans
- ACID RAIN
Nitrogen
Limiting factor- chlorophyll, proteins, amino acids
- atmosphere >78% N
- acid rain, ozone depletion, & climate change
- bacteria= key player in moving nutrients around
Similarities of N to S
- contributes to acid rain
- depends on microbial action to become accessible to plants
Similarities of N to P
-limiting factor for growth (eutrophication)