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Causes, impacts, and sustainability issues of dryland salinity on wetlands in Australia

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Title: Causes, impacts, and sustainability issues of dryland salinity on wetlands in Australia


1
Causes, impacts, and sustainability issues of
dryland salinity on wetlands in Australia
  • SWES 574
  • W. J. Ward
  • 12/09/2003

2
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4
Mining and Agriculture Anthropogenic Salinisation
  • Dryland salinities result from
  • Diverted inflows for irrigation and other uses
  • Excessive clearance of natural, deep rooted
    vegetation from catchments
  • Discharge of saline agricultural wastewater
  • Rising saline groundwater
  • Mining and discharge of brine waters
  • Salinity rising in Mono Lake, CA., Pyramid Lake,
    NV., Aral Sea, Asia, Qinghai Hu, China, Lake
    Qarum, Egypt, Lake Corangamite, AUS. and rivers
    Syr, Amu darya, Asia, Blackwood, AUS.

5
Anthropogenic Salinisation (cont.)
  • Salinisation common in semi-arid regions of
    annual rainfall of 25-500 mm
  • 43-47 of all irrigated land has been effected
    by salinisation
  • Potential to cause irreversible damage to arid
    land rivers and wetlands
  • In Australia lost agricultural production is 50
    mil/yr U.S. and degradation of infrastructure is
    an additional 90 mil/yr. U. S.
  • Vegetation death is caused by toxic levels of
    bicarbonate, magnesium, sulphate, sodium, and
    chloride
  • Loss of species and species diversity
  • Waters become unusable for irrigation or drinking

6
Copper Lode Gold Bauxite Tin
Nickel Uranium
Figure 1 Known Mineral Resources
7
Removal of native vegetation causes increased
recharge to groundwater
Water table rises with increased groundwater
mobilization
Saline Seeps
Dry land Crops and Grazing
Low Permeability layer
Hydraulic Pressure and upward groundwater
movements in aquifers
Saline lake size increases as water table rises
Saline soil develops where water table rises to
less than 2 meters from surface
Saline groundwater in drains
Figure 2. Clearing deep rooted vegetation leads
to salinity of rivers and lakes
8
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11
CEC total amount of exchangeable cations that
can be held by a given mass of soil
12
Exchangeable Ca / Na Cation Experiment
  • Saturate Arizona White House Bt horizon clay with
    NaCl Cations
  • Removed Cl ions by washing
  • Mix clay with sand for permeable layer
  • Flow solution of CaCl2 through clay/sand
  • Remove excess Ca cations and Cl ions by washing
  • Extract Ca cations with LaMotte Extraction
    Solution
  • Precipitate Ca cations with LaMotte Sodium
    Oxalate
  • Compare sample precipitate with LaMotte sample
    strip

13
RESULTS Visually compare test tube results with
PPM chart ? ? ?
Background Ca Na Exchanged 130 mg/L Ca Na
Exchanged in Sat. Ca
14
Figure 3. Dryland Salinity Hazard
Australian rising groundwater salinity sequence
of events dryland salinity hazard mapping using
GIS
  • Tree clearing in upper part of catchment
  • Winter rains with low evapotranspiration
  • Fractured rock deep groundwater aquifer
  • Hydraulic head beneath clay floor
  • Kaolinite, illite, and semectite in debris-flow
    allows cation-exchange releasing sodium
  • Clays decrease hydraulic conductivity under
    saturated conditions

15
Summary
  • Early mining timber use and early settlement and
    agriculture land clearing degraded long term
    sustainability
  • Increased recharge creates valley area
    groundwater discharge through clay debris flow.
  • Discharge cation exchange causes increased
    salinity of surface waters negatively impacting
    lakes and wetlands

16
Summary (cont.)
  • Column experiment simulated the cation exchange
    between Ca Na in high CEC clays
  • Cation exchange occurring in Yass River
    Catchment, New South Wales, Australia causing
    rising salinity in rivers, lakes, and wetlands
  • Mapping salinity and remediation to prevent
    excess infiltration is key to further damage

17
  • Reference List
  • Blinn, D. W. and Bailey, P. C. E.(2001).
    "Land-use influence on stream water quality and
    diatom communities in Victoria, Australia a
    response to secondary salinization."
    Hydrobiologia , 466(1-3), 231-244.
  • Bradd, J. M., Milne-Home, W. A., and Gates,
    G.(1997). "Overview of Factors Leading to Dryland
    Salinity and its Potential Hazard in New South
    Wales, Australia." Hydrogeology Journal, 5(1),
    51-67.
  • Davis, J. A. and Froend, R.(1999). "Loss and
    degradation of wetlands in southwestern
    Australia underlying causes, consequences and
    solutions." Wetlands Ecology and Management,
    7(1-2), 13-23.
  • George, R., McFarlane, D., and Nulsen, B.(1997).
    "Salinity Threatens the Viability of Agriculture
    and Ecosystems in Western Australia."
    Hydrogeology Journal, 5(1), 6-21.
  • Hendricks, D. M. (1985). Arizona Soils, Roswell
    Bookbinding, University of Arizona.
  • Jankowski, J. and Acworth, I. R.(1997). "Impact
    of Debris-Flow Deposits on Hydrogeochemical
    Processes and the Developement of Dryland
    Salinity in the Yass River Catchment, New South
    Wales, Australia." Hydrogeology Journal, 5(4),
    71-88.
  • Johnson, R. H. and Bush, P. W. (2002). "Summary
    of the Hydrology of the Floridan Aquifer System
    In Florida and In Parts of Georgia, South
    Carolina, and Alabama." USGS Professional Papers,
    1403-I.
  • Lemay, T. (2001). "Groundwater Chemistry in the
    Athabasca In Situ Oil Sands Area, Northeast
    Alberta." Rocks Chips, Publication of the Alberta
    Geological Survey, 1-4.
  • Markewitz, D., Davidson, E. A., de O. Figueiredo,
    R., Victoria, R. L., and Krusche, A. V. (2001).
    "Control of cation concentrations in stream
    waters by surface soil processes in an Amazonian
    watershed." Nature, 410, 802-805.
  • McBride, M. B. (1994). Environmental Chemistry of
    Soils, Oxford.
  • Nabhan, G. (1985). Gathering the Desert,
    University of Arizona Press, Tucson, Arizona.
  • Rolls, E. C. (1999). "Land of Grass The Loss of
    Australia's Grasslands." Australian Geographical
    Studies, 197.
  • Tickell, S. J.(1997). "Mapping Dryland-Salinity
    Hazard, Northern Territory, Australia."
    Hydrogeology Journal, 5(1), 109-117.
  • Williams, W. D.(1999). "Salinisation A major
    threat to water resources in the arid and
    semi-arid regions of the world." Lakes
    Reservoirs Research and Management , 4(3-4), 85.
  • Williams, W. D.(2001). "Anthropogenic
    salinisation of inland waters." Hydrobiologia,
    466(1-3), 329-337.
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