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Cycles in nature

Fresh water is purified and reallocated through the hydrological cycle in nature. Nowadays, this natural process is inadequate due to human activities, and specifically because of the thoughtless wasting of water and discharge of various pollutants into the aquatic environment. [Pg.17]

Auclair, J. C. 1995. Implications of increased UV-B induced photoreduction Iron(II) enrichment stimulated picocyanobacterial growth and the microbial food web in clear-water acidic Canadian Shield lakes. Canadian Journal of Fisheries and Aquatic Sciences 52 1782—1788. Auclair, J. C., P. Brassard, and P. Couture. 1985. Total dissolved phosphorus Effects of two molecular weight fractions on phosphorus cycling in natural phytoplankton communities. Water Research 19 1447—1453. [Pg.207]

Each GCC model differs in the set of assumptions made and therefore concentrates on different effects. For instance, a simple numerical model of the gas exchange at the ocean-atmosphere boundary in the case of wind-driven roughness of the sea at wind speeds of 7 m s 1 makes it possible to formulate, in the global model, a unit to calculate the persistent C02 flux between the water surface and the atmosphere. This can be exemplified by models of the ocean carbonate system described by many authors. Also, there are other models of the C02 cycle in natural systems (Riedo et al., 2000 Zonneveld, 1998). [Pg.164]

Numerical models of the global nitrogen cycle 4.4.2.1 Conceptual schemes of the nitrogen cycle in nature... [Pg.229]

Ferguson, J.F. and Gavis, J. A review of the arsenic cycle in natural waters. Water Res. 1259-1274 (1973). [Pg.734]

One of the difficulties in getting information on research already carried out in Brazil is that the dissertations of graduate students in the universities are seldom published in indexed journals. There has been no attempt to compare the cerrados with other savannas in South America, other continents, or Amazon forests because the information available from the cerrados on quantitative aspects of nutrient cycling in natural ecosystems is very meager (Baruch et al. 1996). There are several important studies reported from the Amazon region on nutrient concentrations in plants, litter decomposition, and hydrological cycles over the last couple of... [Pg.68]

Styron, C.E., An assessment of natural radionuclides in the coal-fuel cycle. In Natural Environment III, p. 1511-1520. CONF-780422 (Vol. 2), 1980. [Pg.60]

To exemplify inhibition effects, we choose a few case studies with Fe(III)(hydr)oxides because these oxides are readily dissolved with protons, ligands, and reductants and are of great importance in the iron cycles in natural waters. The reductive dissolution of Fe(III) minerals by a reductant such as H2S is much faster than ligand- or proton-promoted dissolution. The dissolution reaction, as shown by Dos Santos-Afonso and Stumm (1992), is initiated by the formation of =FeS and =FeSH surface complexes the subsequent electron transfer within the complex leads to the formation of Fe(II) centers in the... [Pg.796]

If we are satisfied to omit innumerable details, we can trace, for each of the most important chemical elements concerned, the broad outline of its cycle in nature. The elements and simple compounds principally concerned are carbon (COj), oxygen (O2), nitrogen (Nj, NH3, N02 , N03 ), water (H2O), phosphorous (P04 etc.). .. For the drama of life is like a puppet show in which stage, scenery, actors and all are made of the same stuff. The players, indeed, have their exits and their entrances, but the exit is by way of translation into the substance of the stage and each entrance is a transformation scene. So stage and players are bound together in the close partnership of an intimate comedy and if we would catch the spirit of the piece, our attention must not all be absorbed in the characters alone, but must be extended also to the scene, of which they... [Pg.908]

Fig. 6.4.1. Simplified version of the overall sulfur cycle in nature. The encircled 1 refers to the microbiological cycle while the encircled 2 depicts a food cycle with higher animals. Fig. 6.4.1. Simplified version of the overall sulfur cycle in nature. The encircled 1 refers to the microbiological cycle while the encircled 2 depicts a food cycle with higher animals.
EuUer, C. C., and Davis, J. A., 1989, Influence of coupling of sorption and photosynthetic processes on trace element cycles in natural waters Nature, v. 340, p. 52-54. [Pg.435]

By means of these changes much nitrogen from the animal or vegetable body is again thrown back into the atmosphere in its original form, thus maintaining the nitrogen cycle in nature. [Pg.8]

The carbon cycle in nature uses the energy supplied by sunlight for plants to take atmospheric COj to organic fixed carbon that through various chemical or biological steps goes back to atmospheric CO2. Sugars produced by plants are... [Pg.193]

All elements have cycles in nature, as per Figure 8.2. Sometimes elements are locked in as insoluble organic material in rocks or as inorganic precipitates and it may well be that mobilization can be achieved by the presence of other materials such as an organic ligand. [Pg.111]

Thus we can see that the interactions of biogeochemical cycles in natural waters and relevant ratios between nutrients in various aquatic living organisms determine the productivity of freshwater and marine ecosystems. [Pg.205]

Zehnder, A. J. B., Zinder, S. H. (1980). The sulfur cycle. In Natural environment and Biogeochemical Cycles. Berlin Springer-Verlag, 105-146. [Pg.552]

Figure 1. Outline of metal and ligand cycling in natural waters. Figure 1. Outline of metal and ligand cycling in natural waters.
These ectoenzymes play a significant part in phosphorus cycling in natural waters. In lakes and oceans, phosphorus is partitioned among particulate and dissolved inorganic and organic fractions and is rapidly transformed from one fraction to another. Estimates of the size of the labile dissolved organic phosphorus pool in waters off the coast of Hawaii (0.01-0.2 /rg at P L 1), and its rapid turnover (0.008-0.04 h 1), presumably facilitated by extracellular phosphatases, are comparable with those of PO4- (Smith et al., 1985) and indicate the importance of ectoenzymes in the major nutrient cycles. [Pg.252]

These observations present a strong case for a role of ectoenzymes in manganese and perhaps iron and copper cycling in natural waters. [Pg.254]


See other pages where Cycles in nature is mentioned: [Pg.492]    [Pg.87]    [Pg.578]    [Pg.415]    [Pg.281]    [Pg.736]    [Pg.45]    [Pg.2]    [Pg.126]    [Pg.160]    [Pg.229]    [Pg.243]    [Pg.348]    [Pg.530]    [Pg.1268]    [Pg.136]    [Pg.146]    [Pg.94]    [Pg.3123]    [Pg.183]    [Pg.206]    [Pg.25]    [Pg.240]    [Pg.10]    [Pg.388]   
See also in sourсe #XX -- [ Pg.111 ]




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Natural cycles

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