Abstract
It took us about 180,000 years but finally we did it. We hit Earth’s carrying capacity for hunters and gatherers. That happened more or less 10,000 years ago and in order to keep going forth and multiplying, humanity had to learn how to farm. Talk about a multidisciplinary endeavor. There were plants and animals to be bred, tools to be designed, materials to be discovered, and a whole lot of biology, chemistry, hydrology, geology, meteorology, ecology, and biogeochemistry to be mastered. We’re still working on it (and have added mechanization, transportation, refrigeration, genetic engineering, electronics, and information technology, among other things, to the list). Needless to say, our early stabs at farming were nowhere near as fruitful and reliable nor as intensive and destructive as the farming we do today. But as we slogged through the millennia, growing ever better at farming, ever more of us could be fed. So our numbers kept increasing. Do you see the vicious circle? As long as the human population keeps growing, so must the production of food through farming so that at least some chunk of the population that there has been enough food to produce doesn’t then starve to death. For a long time, much of the getting better at farming meant increasing our control over the landscape and in no small part this was through damming. It also meant increasingly disrupting the biogeochemical cycles of nitrogen and phosphorus in our quest to keep cropland fertilized and productive. Both of these activities have had profound effects on the silica cycle.
Access this chapter
Tax calculation will be finalised at checkout
Purchases are for personal use only
Notes
- 1.
As defined by the International Commission on Large Dams (ICOLD).
- 2.
Earth, on the other hand, has been making massive dams on her own out of ice and out of avalanches, etc., for as long as there has been landscape and water to run through it.
- 3.
Small single-purpose dams can also be used to control the flow of water to mills, to store unwanted and generally hazardous byproducts of mining or other industrial activities, or even (in older times) to release water in a rush that rapidly transports a load of logs downstream and out of the forest.
- 4.
It also means that a lot of these dams are reaching the end of their structurally safe age. Unfortunately, we haven’t set aside money or made much in the way of plans to replace or remove many of them. Knowing the human race, that will probably have to wait until these dams start failing in droves.
- 5.
Yes, indeed, there are such things as freshwater sponges.
- 6.
They divide into two, then two becomes four, and four becomes eight, and so on like in the famous shampoo commercial from the 1970s until you’re up into the millions of phytoplankton cells per liter, quite a lot of biomass.
- 7.
Limnology is the study of inland waters, including rivers, ponds, lakes, reservoirs, wetlands, estuaries, and groundwater, with focus on the interactions between organisms and their environment.
- 8.
Incidentally, Eugene Stoermer was also the co-namer of the Anthropocene.
- 9.
These days we are tending towards using zeolites instead because they don’t add massive amounts of a major nutrient to the water, although by even this very late date, there are few national laws against the use of phosphate in detergents.
- 10.
Using the isotope lead-210 (210Pb), which has a half-life of 22 years and is a particulate material which is continually falling out of the atmosphere following its production by the decay of radioactive radon gas.
- 11.
The addendum here is that the water quality (and dissolved silica content) began improving in the first decades of the twenty-first century due to improvements in sewage treatment and to the phasing out of phosphate detergents. Then the quagga mussel invaded, via larval stages that most likely arrived in water released from the ballast tanks of transoceanic shipping vessels. The quagga and its relatives are voracious filter feeders and they’ve colonized enough of Lake Michigan to keep the waters clear of algal blooms, regardless of the lake’s nutrient status. Unfortunately, this means that phytoplankton still aren’t making it into the food chains that lead to fish, causing a collapse in the lake’s fisheries. Poor Lake Michigan can’t catch a break from the trouble caused by human beings.
- 12.
Larry Mayer and Steven Gloss, two widely known and respected biogeochemists, had first noted the effect on dams on dissolved silica in 1980 in a published paper on the Colorado River in Arizona before and after the construction of Edward Abbey’s favorite of favorites, the Glen Canyon Dam.
Further Reading
Conley DJ, Stålnacke P, Pitkänen H, Wilander A (2000) The transport and retention of dissolved silicate by rivers in Sweden and Finland. Limnol Oceanogr 45:1850–1853
Humborg C, Conley DJ, Rahm L, Wulff F, Cociasu A, Ittekkot V (2000) Silicon retention in river basins: far-reaching effects on biogeochemistry and aquatic food webs in coastal marine environments. Ambio 29:45–50
Maavara T, Dürr H, Van Cappellen P (2014) Worldwide retention of nutrient silicon by river damming: from sparse data set to global estimate. Global Biogeochem Cycles 28:842–855
Schelske CL, Stoermer EF, Conley DJ, Robbins JA, Glover RM (1983) Early eutrophication in the lower Great Lakes: new evidence from biogenic silica in sediments. Science 222:320–322
Syvitski JPM, Vörösmarty CJ, Kettner AJ, Green P (2005) Impact of humans on the flux of terrestrial sediment to the global coastal ocean. Science 308:376–380
Author information
Authors and Affiliations
Corresponding author
Rights and permissions
Copyright information
© 2017 Springer International Publishing AG
About this chapter
Cite this chapter
De La Rocha, C., Conley, D.J. (2017). Silica, Be Dammed!. In: Silica Stories. Springer, Cham. https://doi.org/10.1007/978-3-319-54054-2_8
Download citation
DOI: https://doi.org/10.1007/978-3-319-54054-2_8
Published:
Publisher Name: Springer, Cham
Print ISBN: 978-3-319-54053-5
Online ISBN: 978-3-319-54054-2
eBook Packages: Earth and Environmental ScienceEarth and Environmental Science (R0)