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![]() | ![]() ![]() Jump to: Grade Level: 7-12 Estimated Time: One class period to watch each of the videos. One class period to mix the soil and plant seeds. One month or more to collect data from the plants. One period to graph and analyze the data.
Overview
Teaching Strategy Describe the makeup of the soil in the Amazon and provide a short history of the continent. You may use short segments of "Journey To Amazonia" to show the layers of clay along the Amazon riverbanks. Discuss the lack of nutrients in the Amazon soil and have the students compare potting soil (or soil from your area) with the agricultural clay. Break students into groups of two to four and distribute the planting flats. Planting flats are the containers used by greenhouses to sprout plants; each can accommodate between four and twenty plants, depending on the size of the flat. Students will fill all the sections in one flat with the same kind of soil and label the container. Ideally, each group will grow a flat of plants in each soil type, but soil types may be assigned to groups if space or monetary restraints dictate. One seed should be placed in the center of each section. Students will then take readings over the period of the experiment. Teachers should explain that scientists take large numbers of readings in biology experiments and average results to better insure a correct interpretation of the results. Each group will take their own data and combine it with data from the rest of the class for the final result. Classes that have access to computers will find this is an excellent spreadsheet activity. Students will conclude the exercise by writing a description of their findings in a lab report, or they may present their findings on a poster.
Background The Amazon River is an ancient river that may even have started when South America was joined with Africa. During the last 600 million years, the river has worn the land very flat and removed almost all of the soluble nutrients. The river meanders back and forth, constantly scouring the basin and moving nutrients downstream. It leaves behind almost inert clay as the soil. Soils are divided into layers that are called horizons. The top horizon, the O horizon, is made of fresh and partially decomposed plant materials. In deciduous forests this layer may be fairly thick but in the rainforest, it's quite thin, usually under an inch. The next layer is the A layer which comprises a mixture of mineral particles and some decomposed organic material. In temperate regions this may be several inches to a foot thick, but in the Amazon it is usually no more than an inch. The B horizon is almost entirely rock particles, along with nutrients that have been washed out of the A horizon. This area is quite thick, running into the feet, in most of the United States while it is quite thin in the Amazon. The C horizon is composed of partially weathered bedrock and bedrock. It lies at various depths in the United States but is buried up to 4000 feet deep in the Amazon basin. There are three main soil orders in the Amazon, though much of the basin has not been examined. Under the forest are the ultisols that are composed mainly of kaolinite clay and minerals that are washed from above. It is acidic, contains primarily aluminum compounds and has limited minerals for plant growth. The oxisols are found under some areas and are comprised mainly of kaolinite clay. This is thick, sticky clay that has almost no nutrients available for plants. Under the higher lands that do not flood, a soil type known as spoldsols is found. This is fairly sandy and acidic. Nutrients wash out of it easily, leaving little for plants to use. Thus the people of the Amazon have multiple problems with farming the soil. The clays are relatively acidic, which stunts root development in plants. The clay contains a lot of aluminum that is toxic to plants. Last, the clay is thick, which makes it hard for plant roots and even water to penetrate. Students will simulate the soils of the Amazon by using a mixture of the agricultural clay with a small amount of sand (about 5%) mixed in. Putting a 1 mm layer of decayed leaves across the top will represent the O and A horizons. Teachers should note that when this soil is watered, most of the water will stand on top of the clay rather than pass through. This is normal and explains why the rivers rise and flood in the rainy season since the water cannot soak into the soil. The survival of the plant life in the Amazon depends on the recycling of nutrients. As leaves or plants die and fall, insects and fungus rapidly decompose them. New plants quickly spring up and use the available nutrients. This rapid succession has sustained the plant life for millions of years. When humans come into an area, the land is often cleared of plants. Natives have cut the plants in small areas and burned them to concentrate the nutrients as a simple fertilizer for many years in a procedure called slash-and-burn farming. Given the lack of minerals, this produced a land that yielded crops for a short time before becoming depleted and forcing the people to move elsewhere. On a small basis, this produced no effect on the basin, but as the population has grown and as foreign corporations establish large-scale farms and ranches in the Amazon, much wider areas are being cut. The result of widespread cutting is to completely remove the nutrients from the area, making recovery impossible. It also allows erosion of the soft clay to occur, choking the waters with silt. In this exercise, students simulate slash-and-burn fertilizer by building a small fire out of wood and other plants, then by mixing the ashes with the top of the clay in one of the flats.
Assessment
Related National Standards
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