The Chesapeake Bay is the most massive estuary in the United States of America.
Spanning lengths over 300,000 meters, this it is a watershed that extends over six states, the District of Columbia, and meets the needs of over 15 million individuals. With its high rate of productivity, its economic and social importance to the surrounding areas, and its close proximity to the U.S. capital, the Chesapeake has the recipient of significant attention for quite some time(Boesch, Donald). One of the issues that threatens this important estuary is eutrophication. For the majority of the 20th century, research, guidelines, and management activity were focused on other issues like wetland loss, over harvesting of fisheries, infectious wastes, etc (Davidson et al, 1997). It took until the final quarter of the century for widespread realization to hit that eutrophication had deteriorated the Bay, with extreme consequences for the Bay’s resources(Malone et al., 1993). After awareness of the impact of eutrophication on water bodies began to increase, when it came to making policies and managing the Chesapeake Bay, eutrophication reduction took precedence over any other issues. As the Bay remains a very important body of water, the significance of understanding one of the major processes responsible for its degradation remains as well. This paper aims to understand the contributing factors of eutrophication in the Chesapeake Bay, with a special focus on the effects of air and