InTeGrate Modules and Courses >Water Science and Society > Student Materials > Unique Properties of Water > The Structure of Water: Properties > The Universal Solvent
InTeGrate's Earth-focused Modules and Courses for the Undergraduate Classroom
showLearn More
These materials are part of a collection of classroom-tested modules and courses developed by InTeGrate. The materials engage students in understanding the earth system as it intertwines with key societal issues. The collection is freely available and ready to be adapted by undergraduate educators across a range of courses including: general education or majors courses in Earth-focused disciplines such as geoscience or environmental science, social science, engineering, and other sciences, as well as courses for interdisciplinary programs.
Explore the Collection »
show Download
The student materials are available for offline viewing below. Downloadable versions of the instructor materials are available from this location on the instructor materials pages. Learn more about using the different versions of InTeGrate materials »

Download a PDF of all web pages for the student materials

Download a zip file that includes all the web pages and downloadable files from the student materials

For the Instructor

These student materials complement the Water Science and Society Instructor Materials. If you would like your students to have access to the student materials, we suggest you either point them at the Student Version which omits the framing pages with information designed for faculty (and this box). Or you can download these pages in several formats that you can include in your course website or local Learning Managment System. Learn more about using, modifying, and sharing InTeGrate teaching materials.

The Universal Solvent

This is, of course, another key property of water because more substances dissolve in water than any other common liquid. This is because the polar water molecule enhances "Dissolving Power." Dissolution involves breaking "salts" into component "ions." For example, NaCl (common salt) breaks down into the ions Na+ and Cl- because of the attraction for ions (atoms or groups of atoms with a charge) to water molecules is high.

Cations, such as Na (Sodium) have a net positive charge, whereas anions (such as Cl, Chloride) have a net negative charge. There are many individual elements and compounds that form ions. Thus, water can hold considerable concentrations of various chemical species depending on their particular properties. Note how the water molecules surround the individual ions, keeping them isolated from other ions in solution. This occurs until the capacity of water to isolate the ions is exceeded, at which point the solution is "saturated" with those ions and cannot dissolve more (salt will begin to precipitate—form a solid).

Learning Checkpoint

Note: The questions below are not graded. They may show up as summative evaluation questions on mid-term or final exams.

1) Which of the following statements is/are correct with regard to the high latent heat of vaporization of water?

  1. In order to evaporate water (convert liquid to vapor or steam) additional energy needs to be supplied to break hydrogen bonds between water molecules, and evaporation causes cooling.
  2. Water evaporates readily at any temperature as long as relative humidity is low.
  3. When vapor condenses, heat is given off because of the re-association of water molecules through hydrogen bonding.
  4. The latent heat of vaporization is a major mechanism of heat transport from low to high latitudes.
  5. All of the above.

2) The heat capacity of water

  1. is much lower than for rock or sand
  2. has little influence on local climate
  3. is higher than most solid or liquid substances
  4. at times causes boiling of surface waters at the equator
  5. none of the above

3) The density of water

  1. is constant throughout the Earth surface temperature range
  2. increases with increasing temperature causing sea level to fall
  3. decreases with increasing temperature causing sea level to rise
  4. cannot be determined accurately by scientists
  5. none of the above

4) Relatively deep temperate-zone lakes, like the Great Lakes, overturn seasonally because

  1. strong winds blow surface waters downward
  2. ice sinks to the bottom, forcing deep waters upward
  3. plankton blooms during summer cause surface waters to be more dense
  4. the maximum density of fresh water is reached at about 4 °C
  5. all of the above

These materials are part of a collection of classroom-tested modules and courses developed by InTeGrate. The materials engage students in understanding the earth system as it intertwines with key societal issues. The collection is freely available and ready to be adapted by undergraduate educators across a range of courses including: general education or majors courses in Earth-focused disciplines such as geoscience or environmental science, social science, engineering, and other sciences, as well as courses for interdisciplinary programs.
Explore the Collection »