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Limnology

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Limnology is the scientific study of inland aquatic ecosystems.

Lake Hawea, New Zealand
Lake Hawea, New Zealand

This field examines the biological, chemical, physical, and geological traits of water bodies. These systems can be fresh or saline, and they can be natural or man-made. Limnologists study diverse environments like lakes, reservoirs, ponds, rivers, streams, wetlands, and even groundwater. Water systems are often categorized by their movement. Lotic systems are running waters, such as rivers. Lentic systems are standing waters, such as lakes. Limnology also looks at the entire drainage basin to see how water and nutrients move through it.

Physical properties shape how these ecosystems function. The morphometry, or shape and structure, of a water body depends on its type and the surrounding geology. For example, lakes are classified by how they formed. In rivers, morphometry is driven by geology and water velocity. Light also creates distinct layers called light zonation. The photic zone, or euphotic zone, is the upper layer where enough sunlight penetrates for plants to grow. Below this is the aphotic zone, where light is too dim for plant growth. This light availability significantly impacts the behavior of organisms like zooplankton.

Temperature also creates distinct layers in a lake, a process called thermal stratification. This creates three main sections based on heat. The epilimnion is the top layer that absorbs solar radiation to stay warm. Below this is the thermocline, where water temperatures drop very rapidly. The bottom layer is the hypolimnion, which is the coldest because it is deep and dark. In temperate lakes, cooling in the fall causes a turnover. This is when the layers mix and the temperature becomes more uniform. In very cold climates, lakes can experience inverse thermal stratification during the winter.

Lake metabolism cross section
Lake metabolism cross section

The chemical makeup of water is influenced by many natural processes. Precipitation, soil, bedrock, erosion, and evaporation all play a role. Carbon comes from two main sources. Allochthonous carbon comes from outside the system, like soil or plants. Autochthonous carbon is produced within the system, such as by algae. In small streams, allochthonous carbon is usually the main source. In large lakes, autochthonous carbon tends to dominate. These chemical processes determine the overall water quality and the health of the ecosystem.

Oxygen and carbon dioxide are closely linked through biological reactions. Autotrophic organisms, like algae, perform photosynthesis. This process uses carbon dioxide and releases dissolved oxygen. Other living things perform aerobic respiration, which consumes oxygen and releases carbon dioxide. Because photosynthesis requires light, it mostly happens during the day. Respiration happens both day and night. This balance is known as the aquatic metabolism rate. If oxygen levels drop below 2 milligrams per liter, the water is called hypoxic. If oxygen reaches 0 milligrams per liter, the water is anoxic.

Lake George from village beach
Lake George from village beach

Nutrients like nitrogen and phosphorus are essential for life. Nitrogen is usually present as a dissolved gas, but most organisms prefer using nitrate, nitrite, or ammonia. Phosphorus is also a critical nutrient, but it is often a limiting factor. This means that low concentrations of phosphorus can limit how much phytoplankton grows. Limnology also explores newer sub-disciplines. Landscape limnology studies the connections between an aquatic ecosystem and its entire drainage basin. Global limnology looks at how inland waters function as part of the Earth system.

Lake Hawea, New Zealand
Lake Hawea, New Zealand

The history of limnology began with François-Alphonse Forel. He coined the term and studied Lake Geneva. He originally described limnology as "the oceanography of lakes." In 1922, August Thienemann and Einar Naumann helped expand the field by co-founding the International Society of Limnology. Later, prominent scientists like G. Evelyn Hutchinson worked in the United States. At the University of Wisconsin-Madison, several researchers helped develop the Center for Limnology. These discoveries have allowed us to understand how inland waters connect to the wider world.

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File:Lake Hawea, New Zealand.jpg
Lake Hawea, New Zealand.jpg
File:Lake metabolism cross section.png
Lake metabolism cross section.png
File:Lake George from village beach.jpg
Lake George from village beach.jpg
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