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Groundwater discharge zone

Hines, M. E., Lyons, W. B., Lent, R. M., and Long, D. T. (1992). Sedimentary biogeochemistry of an acidic, saline groundwater discharge zone in lake tyrreU, victoria, australia. Chem. Geo. 96(1—2), 53-65. [Pg.981]

Arakel, A.V. (1991) Evolution of Quaternary duricrusts in Karinga Creek drainage system, central Australia groundwater discharge zone. Australian Journal of Earth... [Pg.38]

Jacobson, G., Arakel, A.V. Chen, Y. (1988) The central Australian groundwater discharge zone evolution of associated calcrete and gypcrete deposits. Australian Journal of Earth Sciences 35, 549-565. [Pg.358]

In environments where the fluid pressure is decreasing, i.e., where groundwater is moving up, such as at discharge zones. [Pg.84]

Figure 2.1 Settings for calcrete development. In fluvial settings pedogenic calcretes can develop on floodplains and terraces, whereas groundwater calcretes may form in channel deposits or around the capillary fringe and upper part of the phreatic zone in more permeable parts of the floodplain. In alluvial fans paired calcretes may develop on the fans, with hydromorphic calcretes near discharge zones. Figure 2.1 Settings for calcrete development. In fluvial settings pedogenic calcretes can develop on floodplains and terraces, whereas groundwater calcretes may form in channel deposits or around the capillary fringe and upper part of the phreatic zone in more permeable parts of the floodplain. In alluvial fans paired calcretes may develop on the fans, with hydromorphic calcretes near discharge zones.
Burnett WC, Aggarwal PK, Bokuniewicz H, et al. (2006) Quantifying submarine groundwater discharge in the coastal zone via multiple methods. Science of the Total Environment 367 498-543. [Pg.473]

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See also in sourсe #XX -- [ Pg.10 , Pg.11 , Pg.122 , Pg.340 , Pg.352 ]



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