Lakes always die. Their life span is determined by the physical, chemical and biological conditions to which they are subject. Lakes begin by being oligotrophicnearly sterile-with clear, clean water. Gradually silt and nutrients are added. Some of the nutrients come from minerals leached from the sides and bottom of the lake or from organic materials. Silt, other minerals and organic materials come from streams supplying the lake. Eventually the nutrients stimulate increased plant growth, and the character of animal life in the lake changes. In time the mass of new mineral and biological material fills the lake and it becomes a marsh. From marshes, lakes finally become solid land. The whole process is called eutrophication. Without man's interference, the time span for eutrophication is measured in tens of thousands of years or longer, depending on individual conditions. Man, by adding his nutritive wastes to lakes, has compressed the process, sometimes into the space of a few years. The classic case is Lake where the process of eutrophication has indeed been immensely accelerated. But many other lakes, in North America and all over the world, have also become eutrophic because of man's activities. Fortunately, the process is very often reversible; several area report progress. Eutrophication is a complex process, varying from lake to lake in its character, rates and causes. But in most eutrophic bodies of water in the United States, the limiting nutrients are compounds of phosphorus or nitrogen, with phosphorus apparently the more important contributor in most cases. A limiting nutrient is one that acts as an accelerator or decelerator of eutrophication as its amounts are increased or decreased. All other essential nutrients exist in sufficient quantities for more or less unlimited growth, and the limiting nutrient becomes the controlling factor. Although phosphorus is usually the limiting nutrient in North American lakes, sometimes nitrates play the key role, as is apparently the case in Lake Tahoe, on the California-Nevada border. Sometimes nitrogen and phosphorus act together as limiting nutrients. Nitrogen and phosphorus are the main elements causing eutrophication in Lake Erie, says Dr. Frank K. Wilkes of the Federal Water Quality Administration research division in Washington, D.C. He adds, however, that organic materials are also sometimes suspected of being the key nutrients. Scientists use certain standard parameters to gauge the degree of eutrophication in a body of water. Because of the key role nitrogen and phosphorus play, the amounts of these two substances provide a frequently used guideline. Because stimulation of plant growth is a prime effect of eutrophication, the amount of chlorophyll in a lake is another commonly used parameter, as is a simple measurement of the weight of plant growth per acre. The number of plant cells per milliliter of water is .M