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  The Ecology and Chemistry of Water      

 



Feather and frost

Joel Sartore

 

Text excerpted, by permission, from The Nature of Nebraska: Ecology and Biodiversity, by Paul A. Johnsgard '55.

 
Although it has been written that we are but dust and to dust we shall return, it would be far more accurate to say that we came from water (our human bodies are nearly two-thirds water) and to water we must eventually return. Water is one of the most abundant compounds on Earth and one of the most critical components for sustaining life on this planet. It is also one of the most remarkable substances. No other common inorganic material is fluid at temperatures that support life, making it possible for floating and swimming organisms to have evolved and become mobile. Although fluid, the viscosity of water allows for rowing or undulating body movements to provide for easy mobility. Additionally, few natural compounds are so resistant to temperature changes (its so-called specific heat), which helps buffer living cells from rapid, perhaps fatal heating and cooling and also limits the rate of evaporation. Water dissolves essentially all the critical elements needed for life, including all the basic nutritional salts as well as vital gasses such as oxygen, hydrogen, and carbon dioxide. Its biochemical presence is also needed for facilitating all the basic photosynthetic and respiratory processes of living cells that involve carbon, oxygen, and hydrogen.

Although water becomes denser as it cools and approaches freezing, it actually expands as it freezes. Thus ice forms at the tops of lakes and rivers first, rather than from the bottom up. This curious fact allows aquatic organisms to survive in a fluid environment while separated from subfreezing atmospheric conditions above by a protective ice ceiling, thus enabling them to endure long winters or even more prolonged arcticlike conditions. Although water strongly resists freezing, it easily evaporates and by later condensation is able to spread life-giving moisture across the drier parts of the globe as various forms of precipitation.

Because cold water is relatively dense and sinks and warmer water correspondingly rises, oceans develop vertical cycles. As a result, warmer, low-latitude waters rise and replace sinking polar waters, producing upwellings of deep, dissolved ocean nutrients, access to which would otherwise be forever lost to plants and animals. These oceanic cycles, aided by the energy of planetary spin effects, produce enormous clockwise or counterclockwise surface-level currents such as the Gulf Stream, which may either warm or cool adjoining land masses, causing offshore or onshore winds and resulting in increased or reduced coastal precipitation. Oceanic currents therefore influence large-scale terrestrial wind as well as precipitation variables and thereby control continentwide climatic patterns, as recent cycles of La Niña and El Niño have so effectively proven in recent years.

Even in smaller ecosystems and communities such as lakes, marshes, and temporary wetlands, water strongly influences and ultimately controls local species diversity and the overall abundance of plants and animals. This control is largely brought about by the influence of available water in allowing photosynthesis to proceed and thus regulate the initial plant production and subsequent storage of organic matter such as carbohydrates. These materials are then successively funneled through food chains in a predictable and diminishing sequence of exploitation by consumer organisms such as herbivores and carnivores. The consumers in turn are ultimately exploited and transformed back again into their inorganic compounds by lowly decomposer organisms such as bacteria. In short, the water that helped to convert carbon dioxide to organic carbon molecules by green plants is again finally released as water in the process of respiration and decomposition by both plants and animals. As stated earlier, water we are and to water we shall return.

Of all the wonders of Earth, nothing is more valuable than water; without it Earth would be as lifeless as Mars. Nevertheless, nothing on our planet seems to be wasted so flagrantly or polluted so recklessly by humankind as water. Ultimately, we earthlings will have to decide if we wish to share Mars’s fate; postulated interplanetary attempts by NASA to reach and colonize it and to use its possible subsurface ice supplies for human consumption and industrial purposes would be roughly comparable to visiting Earth as it may have appeared 3 billion years ago and hoping to set up a profitable car-wash operation there. It would seem that conserving water on Earth is far simpler, much more profitable, and immensely more critical to our own survival than hoping to find and extract water on Mars.

By permission of the University of Nebraska Press. © 2001 by the University of Nebraska Press. Available wherever books are sold or from the University of Nebraska Press, 800.526.2617, and on the Web at nebraskapress.unl.edu.


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