|
Lesson Plans Units: Oceanography
|
Marine Biology Ocean Topography and Zonation Activity
Introduction During days one and two of this lesson, we filled in unlabeled diagrams of the following during a class discussion:
(Sumich, 1992) During the labeling process, we discussed why there are large-scale features (plate tectonics), climactic zones (planet tilt and heating), and environmental zones (water depth, substrate/no substrate, light availability). Now after dividing into four different groups, (one for each diagram), you will construct scale 3-D models of your group’s assigned diagram, and will be evaluated according to a teacher- made grading scale. When you are done, your model will be presented to the class. Materials Any arts and crafts materials that you or the teacher provides Procedure
Model Building Evaluation Standards Scale, Neatness
and Accuracy
Score 0 through 5 for each category. Score 0 through 5 for participation (from teacher observations). Add total (out of a possible 20). Multiply score times 2 for final grade (out of a possible 40).
Some Physical and
Chemical Properties of Seawater Introduction Compared to most terrestrial environments, the ocean is a relatively stable medium in which to live. Conditions such as temperature and salinity characteristically fluctuate only slightly over daily or even seasonal cycles. Nevertheless, the variations that do exist, however subtle, are extremely important in determining the type and distribution of organisms that are found. In this lab you will discover some properties of water and how those properties are affected by certain conditions. Properties of Water Density Density is a property of all types of matter, including water. Precisely defined, density is the ratio of the mass of a substance to its volume. For instance, we may take 100 lbs. of styrofoam and 100 lbs. of lead and recognize that their weights are the same. Yet, when we compare a unit of volume of each, say a cup, we recognize that a cup of lead weighs more than a cup of styrofoam. Hence, lead has a greater density than styrofoam. Pure water is defined as having a density of 1.00 g/cm3 (or g/ml) at 4° C. The density of seawater varies from place to place in the ocean, depending on evaporation and rainfall rates, river runoff, and water temperature. The density of the water in which they live influences several aspects of the lives of marine organisms. Also, sinking masses of higher density seawater carry oxygen-rich waters from the surface to greater depths, as less dense nutrient-rich water moves upward. Salinity Salinity refers to the total amount of dissolved salts in water in parts per thousand (ppt). Salinity values range from near zero at the mouths of rivers to over 40ppt in the Red Sea. Open ocean salinity values range from about 32 to 36ppt. Procedure
a) The water from the Mediterranean Sea may have a salinity of 39ppt due to excessive evaporation, while the Atlantic Ocean near the Straits of Gibraltar may have a salinity of about 36ppt . In the summer, seawater temperatures in the Mediterranean Sea may be about 18° C while Atlantic Ocean temperatures average around 20° C off the mouth of the Mediterranean. Using the provided figure, determine the density of the water from the Mediterranean Sea in the summertime. What is the density of the Atlantic Ocean during the summer also? How will these two masses of water behave when they encounter one another? Why? b) What would happen when a cold Alaskan river runs into the Bering Sea? Assume the river has a temperature of 4° C and the Bering Sea has a temperature of 9° C and a salinity of 33ppt. What will be the density of the river? (What must you assume about the salinity of the river?) What will be the density of the Bering Sea? How will these two water masses behave when they encounter one another? Why?
Lab Reports Evaluation Standards
During this course, you are expected to keep an up-to-date lab notebook that reports and summarizes your findings for each lab session. You must provide a 9 ½" x 6" spiral. The purpose of this book is to help you organize and to keep track of all results and conclusions as we work. Writing down scientific observations helps to make you think and analyze about what you are working on. Your notebook will be turned in and graded after each lab session. Reporting Rules 1) Each lab must be started on a new, clean page. Write on one side of the paper only. 2) When making observations, write down exactly what YOU see. Use adjectives to make accurate and useful descriptions. You may discuss observations among your lab partners before you write them down. 3) BE NEAT! Organize your information into sections. (See reporting format below). Don't get chemicals or water on your book. Use legible handwriting. DON'T scribble sketches--go for detail. 4) Use third person only. (NO me, we, you, I, us…) 5) Use the following format to formally report your hypothesis, procedure, data and conclusions. Reporting Format 1) Title each new lab. 2) Each lab is divided into the following sections. Label each section as you go and write in paragraph style" the information required for each part. A) PURPOSE: What is the lab all about? What are the goals of the lab and why are they important? What will it help you to understand? What are you to be looking for? What is the hypothesis? What predictions did you make from that hypothesis? B) PROCEDURE: Summarize the experimental procedure you used, being specific to amounts used and to what types of observations were made. (If someone wanted to repeat your work, could they do it exactly as you did?) C) DATA: Organize data into labeled tables and graphs. Neatly make any required sketches, making sure to label when required. (Colored pencils are highly recommended). Written observations belong here also. D) CONCLUSIONS: Do your results confirm or contradict your hypothesis? Why or why not? How could you redo the experiment to make it better or reword the hypothesis? Also answer any required questions that the teacher has assigned. 3. Try to go above and beyond what is required above in order to get an "A+" grade. Don't try to just get away with the bare minimum. (Don’t try to add a bunch of nonsense filler just to get your lab to be longer. "Baloney" does not impress me - conciseness does). You will be assigned subjective "quality points" by the teacher for this. Grading Organization (5 points total)
Purpose (10 points total)
Procedure (5 points total)
Data (10 points total)
Conclusion (15 points total)
Quality Points (up to 5 points extra credit)
The grade is out of a possible 45 points. The Ocean in Motion Activity Introduction During day one of this lesson we had a class discussion to come up with the different ways in which water moves and we came up with the following list:
You were then allowed to speculate as to:
You will now organize into five groups, be assigned a water motion type and construct a graphic display, (a concept map) about your topic. When you are done, your graphic display will be presented to the class as you teach the class about your type of water motion and the class will then take a quiz that you devised. You will be evaluated according to a teacher made grading scale. Materials
Procedure
Concept Map Evaluation Standards Content, Neatness
and Accuracy
Score 0 through 5 for each category. Score 0 through 5 for participation (from teacher observations). Add total (out of a possible 20). Multiply score times 2 for final grade (out of a possible 40) The
University of Arizona
Department of Biochemistry and Molecular Biophysics General Biology Program for Secondary Teachers warder@email.arizona.edu http://biology.arizona.edu/sciconn/lessons2/lessons.html
|