Chapter 5.docx

5 Pages
112 Views
Unlock Document

Department
Environmental Science
Course
EESA01H3
Professor
Carl Mitchell
Semester
Summer

Description
Chapter 5 (week 3) Eutrophication: is the movement of a body of water′s trophic status in the direction of increasing plant biomass, by the addition of artificial or natural substances, such as nitrates and phosphates, through fertilizers or sewage, to an aquatic system. Cycle: shape the landscapes around us and guide the flow of key chemical elements and compounds that support life and regulate climate. Open system: Systems that receive inputs of both energy and matter and producer outputs of bot. Closed system: Systems that receive inputs and produce outputs of energy, but not matter. Feedback loop: Sometimes a system’s output can serve as input to that same system. Feedback loops are of two types, negative and positive. Negative feedback loop: Output that results from a system moving in one direction acts as input that moves the system in the other direction. Positive feedback loop: Have the opposite effect. Rather than stabilizing a system, they drive it further toward on extreme or another. Homeostasis: The tendency of a system to maintain constant or stable internal condition. Steady state: Homeostatic systems are often said to be in a stable or steady state. Emergent properties: Characteristics nor evident in the components alone. Lithosphere: Is the rock and sediment beneath our feet, I the planet’s uppermost layers. Atmosphere: is composed of the air surrounding our planet. Hydrosphere: Encompass all water, salt or fresh, liquid, ice, or vapour in surface bodies, underground, and in the atmosphere. Biosphere: consists of the total of all the planet’s living organisms and the abiotic (nonliving) portions of the environment with which they intersect. Rock cycle: Rocks and minerals that compose them are heated melted, cooled, broken down, and reassembled in a very slow process. Manga: All rocks can melt. At high enough temperatures, rock will enter a molten, liquid sate. Intrusive or plutonic rock (rock-granite): Magma that cools slowly and solidifies while it is still well below Earth’s surface. Extrusive or volcanic rock (rock-basalt): In contrast, when magma is ejected from a volcano, it cools very quickly, so minerals have little time to grow into coarser crystals. Sediments: Particles of rock blown by wind or washed away be water finally come to rest downhill, downstream, or downwind from their sources. Sedimentary rock (rock-limestone and rock-sandstone): is formed when dissolved minerals seep through sediment layers and act as a kind of glue, called cement, which crystallizes and binds the sediment particles together. Lithification: is the process in which sediments compact under pressure, expel connate fluids, and gradually become solid rock. Essentially, lithification is a process of porosity destruction through compaction and cementation. Lithification includes all the processes which convert unconsolidated sediments into sedimentary rocks. Petrification, though often used as a synonym, is more specifically used to describe the replacement of organic material by silica in the formation of fossils. In geology consolidation is a synonym for lithification. Metamorphic rock (rock-gneiss (make up the Canadian Shield)): When great heat or pressure is exerted on rock, the rock may change its form. Plate tectonics: a process that underlies earthquakes and volcanoes and that determines the geography of Earth’s surface. Earth’s surface consists of a lightweight thin crust of rock floating atop a malleable mantle, which in turn surrounds a molten heavy core made mostly of iron. Divergent plate boundaries: Manga surging upward to the surface divides plates and pushes them apart, creating new crust as it cools and spreads. Transform plate boundary: When two plates meet, the may slip and grind alongside one another and creating fiction that spawns earthquakes along slip-strike faults. Convergent plate boundaries: Either of two consequences may result. First, one plate of crust may slide beneath another in a process called subduction. The subducted crust is heated as it dives into the mantle, and it may send up magma that erupts through the surface in volcanoes. Ecosystem: An ecosystem of all organism and nonliving entities that occur and interact in a particular area at the same time. Biomass: Organisms at higher tropic levels, transferring energy, organic material
More Less

Related notes for EESA01H3

Log In


OR

Join OneClass

Access over 10 million pages of study
documents for 1.3 million courses.

Sign up

Join to view


OR

By registering, I agree to the Terms and Privacy Policies
Already have an account?
Just a few more details

So we can recommend you notes for your school.

Reset Password

Please enter below the email address you registered with and we will send you a link to reset your password.

Add your courses

Get notes from the top students in your class.


Submit