Blackwater river

A blackwater river is a river with a deep, slow-moving channel that flows through forested swamps and wetlands. As vegetation decays in the water, tannins are leached out, resulting in transparent, acidic water that is darkly stained, resembling tea or coffee. Most major blackwater rivers are in the Amazon River system and the Southern United States. The term "blackwater" here is an agreed-upon technical one in fluvial studies, geology, geography and ecology/biology. Not all dark-colored rivers are true blackwater rivers in the technical sense. Some rivers in temperate regions, which drain or flow through areas of dark black loam, are colored black due to the color of the soil. These types of rivers can be referred to as black mud rivers; there are also black mud estuaries (see link above to rivers officially named Blackwater River.)

Blackwater rivers are much lower in nutrients than whitewater rivers and have ionic concentrations only slightly higher than rainwater.[1][2] The unique water conditions lead to a composition of flora and fauna that differs significantly from that found in whitewater sources. Areas where blackwater rivers and whitewater rivers combine are particularly attractive to a diverse group of organisms.

Contents

Comparison between white and black waters

Table 1: Mean ionic composition, specific conductivity (μS/cm), and pH in Amazon waters.[3]
Solimões or Amazon River – whitewater. Rio Negro – blackwater.
Na (mg/L) 2.3 ± 0.8 0.380 ± 0.124
K (mg/L) 0.9 ± 0.2 0.327 ± 0.107
Mg (mg/L) 1.1 ± 0.2 0.114 ± 0.035
Ca (mg/L) 7.2 ± 1.6 0.212 ± 0.066
Cl (mg/L) 3.1 ± 2.1 1.7 ± 0.7
Si (mg/L) 4.0 ± 0.9 2.0 ± 0.5
Sr (μg/L) 37.8 ± 8.8 3.6 ± 1.0
Ba (μg/L) 22.7 ± 5.9 8.1 ± 2.1
Al (μg/L) 44 ± 37 112 ± 29
Fe (μg/L) 109 ± 76 178 ± 58
Mn (μg/L) 5.9 ± 5.1 9.0 ± 2.4
Cu (μg/L) 2.4 ± 0.6 1.8 ± 0.5
Zn (μg/L) 3.2 ± 1.5 4.1 ± 1.8
Conductivity 57 ± 8 9 ± 2
pH 6.9 ± 0.4 5.1±0.6
Total P (μg/L) 105 ± 58 25 ± 17
Total C (mg/L) 13.5 ± 3.1 10.5 ± 1.3
HCO3-C (mg/L) 6.7 ± 0.8 1.7 ± 0.5

Black and white waters differ significantly in their ionic composition, as shown in Table 1. Black waters are much more acidic, resulting in an aluminium concentration greater than that of the more neutral white waters. The major difference is the concentrations of sodium, magnesium, calcium and potassium; these are very low in black waters. This has considerable ecological implications. As some animal groups, such as snails, need much calcium with which to build their shells, they are not abundant in black waters. The lack of dissolved ions in black waters results in a low conductivity, similar to that of rainwater.

Black and white waters also differ in their planktonic fauna and flora. Tables 2 and 3 compare the number of planktonic animals caught in black and white water localities only a few meters apart. In fact, the black water was not as extreme an example as can be found in the Rio Negro system. However, it can be seen that the black water held far greater numbers of rotifers but fewer crustaceans and mites. These crustaceans are important foods for larval fish. The zones where the two waters mix are particularly attractive to ostracods and young fish. These mixing zones tend to have high numbers of animals. The high abundance of animals is shown clearly in Table 3, which compares the numbers of animals present in 10 litres of water in each habitat sampled.[4]

Table 2: Different planktonic organisms collected in black (Japura) and white (Solimoes) waters.[3]
Animal groups present Black water Mixed water White water
Rotifera 284 23 0
Cladocera 5 29 43
Ostracoda 39 97 29
Calanoida 11 51 66
Cyclopoida 22 49 61
Chironomidae 0 3 3
Acari (mites) 0 0 2
Table 3: Number of planktonic organisms collected in 10 L of black, white and mixed waters.[3]
Black water Mixed water White water
Animal groups present Open water Forest Open water Forest Open water Forest
Volvocaceae 42   38      
Rotifera 87 5 34      
Cladocera 6   5   8 1
Ostracoda 2 11 3   7  
Calanoida 23 3 10      
Cyclopoida 5 27 19 1 13 1
Mysidacea   1        
Diptera         1  
Acari (mites)     1   1  
Larval fish     1   1  

Blackwater rivers of the world

Indonesia

Amazonia

Orinoco basin

Southern United States

St. Marys River (Georgia): http://www.saintmarysriver.org/history.html

Northern United States

Australia

Europe

Images of blackwater rivers

See also

References

  1. ^ Janzen, D H (July 1974). "Tropical Blackwater Rivers, Animals, and Mast Fruiting by the Dipterocarpaceae". Biotropica 6 (2): pp. 69–103. doi:10.2307/2989823. JSTOR 2989823. 
  2. ^ Sioli, Harald (1975). "Tropical rivers as expressions of their terrestrial environments". Tropical Ecological Systems/Trends in Terrestrial and Aquatic Research (New York City: Springer-Verlag): pp. 275–288. 
  3. ^ a b c J S B, Ribeiro; A J Darwich (1993). "Phytoplanktonic primary production of a fluvial island lake in the Central Amazon (Lago do Rei, Ilha do Careiro)". Amazoniana (Kiel) 12 (3-4): pp. 365–383. 
  4. ^ "Comparison between white and black waters". Amazonian Fishes and their Habitats. Pisces Conservation Ltd. http://www.amazonian-fish.co.uk/indexc30.html. Retrieved 2006-05-21.