Title: Causes, impacts, and sustainability issues of dryland salinity on wetlands in Australia
1Causes, impacts, and sustainability issues of
dryland salinity on wetlands in Australia
- SWES 574
- W. J. Ward
- 12/09/2003
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4Mining 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.
5Anthropogenic 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
6Copper Lode Gold Bauxite Tin
Nickel Uranium
Figure 1 Known Mineral Resources
7Removal 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
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11CEC total amount of exchangeable cations that
can be held by a given mass of soil
12Exchangeable 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
13RESULTS 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
15Summary
- 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
16Summary (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
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