In science, the term "transport" refers to the movement of substances (such as water, nutrients, gases, and waste products) within living organisms and between different parts of an organism. This movement is essential for the survival and proper functioning of cells, tissues, and organs.
Active Transport: This is the movement of molecules across a cell membrane against the concentration gradient, requiring the expenditure of energy (usually in the form of ATP).
Facilitated Diffusion: This is a type of passive transport that involves the use of transport proteins to allow specific molecules to cross the cell membrane.
Osmosis: This is the diffusion of water across a selectively permeable membrane, from an area of lower solute concentration to an area of higher solute concentration.
Here are some key concepts to focus on when studying the topic of transport:
Understand the different types of transport mechanisms in living organisms, including diffusion, active transport, facilitated diffusion, osmosis, and bulk transport.
Be able to explain the role of transport systems in plants, including the functions of xylem and phloem.
Describe the structures and functions of the circulatory and respiratory systems in animals, and how they facilitate the transport of substances throughout the body.
Explore the importance of transport in maintaining homeostasis and supporting the overall health and function of living organisms.
Remember to review diagrams and illustrations that depict the processes of transport, as visual aids can help in understanding the complex mechanisms involved.
Earth/Space Science: Students will use scientific skills and processes to explain the chemical and physical interactions (i.e., natural forces and cycles, transfer of energy) of the environment, Earth, and the universe that occur over time.
Earth History: Explain how sedimentary rock is formed periodically, embedding plant and animal remains and leaving a record of the sequence in which the plants and animals appeared and disappeared.
Explain how sedimentary rock buried deep enough may be reformed by pressure and heat and these reformed rock layers may be forced up again to become land surface and even mountains.