IRRIGATION AUSTRALIA WEBSITE Channel Seepage Management Tool (Please click to return to home page)

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Seepage risk, potential

Identification & measurement

General issues

Recom. approach &
techniques

Techniques

Inflow-outflow tests

Pondage tests

Point measurement

Soil & geological profile

Groundwater
assessment

Geophysical surveys

Remote sensing

Remediation

Remediation costs, benefits

Prioritisation of works

Project review

Case studies

Downloads

Glossary

References

Techniques for identification and measurement

This website provides information on how to conduct seepage measurements using techniques considered most relevant to Australian conditions and operations. As well as an understanding of how to actually undertake the tests there are some basic project considerations (see 4 Selection of seepage measurement techniques for more information).

What seepage measurement techniques are available?

Seepage measurement techniques include direct and point seepage measurement, subsurface characterisation, and remote non-invasive techniques.

Seepage identification & measurement techniques

Scale [1]

Operational constraints Accuracy Cost Best suited
to...
Local Inter-
mediate
to large
Macro
Direct & point measurement The techniques most likely to provide accurate measurements of the rate of seepage are pondage tests and inflow-outflow tests. In addition, point measurements provide a way of quantifying seepage rates at specific locations in a channel.
Inflow-outflow tests   Very minimal effect on operation Fairly accurate over long sections (depending on method of measuring flows) Depends on whether existing structures in place for measuring flow - if not, contractors required & will be moderately expensive Regional to large scale investigations for quantifying seepage at a broad scale
Pondage tests [2]   Must be conducted at start or end of channel run Most accurate method Relatively expensive, largely due to cost of pond bank construction. Investigations requiring seepage rates to a reasonable level of accuracy. Useful for calibrating techniques with greater density of spatial data (eg, soil and geological profile classification, geophysics)
Point measurement     Some types can be conducted while channel running Not reliable for absolute quantification. Depends on density of tests - will be relatively expensive if reasonable level of accuracy required Local scale investigations and assessment of relative seepage [3]
Subsurface character-isation Subsurface characterisation of the area around a channel provides information on which assessments of the sites of seepage can be made
Soil and geological profile classification No effect on operation Provides indication of broad zones of relative seepage [3]. Quantification: provides first cut estimate of seepage only Relatively inexpensive if using existing data / maps. Moderately expensive when drilling & on-site classification required Site characterisation and assistance in interpreting other seepage results.
Groundwater assessment

Including water-level monitoring, mathematical modelling and hydrochemical investigations
  No effect on operation Accurate if aquifer parameters properly characterised, which can be expensive. However only relevant for slice across a channel Moderately expensive, depending on groundwater depth. Aquifer characterisation for quantifying rates likely to be expensive. Most chemical techniques highly expensive. Best at local scale due to intensive data requirements. Provides permanent assessment tool, therefore useful for post-remediation assessment.
Remote non-invasive techniques ‘Direct and point measurement’ and ‘subsurface characterisation’ techniques assist in identification of seepage distribution and rate by directly measuring a physical property at a single location. For example, groundwater monitoring of water levels in a bore allows a direct measure of the watertable, and infiltration tests are direct measures of the soil properties at a point.
In contrast, Geophysical surveys and remote sensing techniques use high-density sampling of subsurface and near-surface properties to provide continuous data along the channel.
Geophysical surveys [2]   No effect on operation Most accurate method for assessing relative seepage2. Most efficient method for quantification of seepage if calibrated, eg against pondage tests Relatively inexpensive in terms of km channel covered but proper interpretation and calibration (eg pondage tests) will increase costs Recommended technique for large scale investigations - when 'calibrated' against pondage tests provides a good indication of relative seepage AND actual seepage rates
Remote sensing   No effect on operation Can accurately detect surface / near surface seepage over large areas, but not useful for seepage quantification Relatively inexpensive (depending on source data used) in terms of km channel covered but proper interpretation will increase costs Large scale to regional investigations where the primary focus is on land degradation (eg, salinity) induced by channel seepage

Notes:
(Numbers in [ ] brackets)

  1. Guidelines for the definition of each scale are:
    Local - approx. 400m
    Intermediate to large - 100's m to tens of kms
    Macro - tens kms to an entire system
    For a more detailed definition of scale see: General issues in channel seepage identification and measurement
  2. The recommended approach for intermediate to large scale investigations involves a combination of pondage tests and geophysical surveys, which allows estimation of seepage rates based on geophysical response via 'calibration' against pondage tests
  3. Relative seepage means that information is provided on whether one section is likely to be seeping at a higher or lower rate compared to another section - no information is provided on the actual magnitude of the rate.
Each of the techniques is presented within the following framework:

Summary

Summary of principle, method, applicability, practical implementation, experience from the trials, indicative costs

Principle

Outlines how the technique is used to indicate and measure seepage.

Method

How to undertake the technique. Describes the set-up, planning, operation, collection and analysis of data and descriptions of the way in which results are presented and used, based largely on examples from the IAL trials. Worked examples of calculations are provided.

Descriptions include some of the practical and contractual issues to be considered in implementing the measurement techniques

Applicability

Reason for using the technique (advantages and disadvantages). Refers to the outcomes likely to be obtained and how these meet project objectives. It embraces factors such as scale and physical conditions (soil, groundwater, etc.). It also applies to techniques for post-remediation measurement and monitoring.

Practical implementation

Factors to be considered before implementation. Identifies factors such as scale, timing of testing, and operational and physical constraints on undertaking the technique at a particular site.

Experience from the Trials

Experience implementing the technique including case studies.

Indicative costs

Costs based on various situations. Summarises indicative costs to set up, implement, monitor and analyse the information. Costs of interpretation and input to channel management are not included as these are pertinent to the individual channel operator.

Indicative costs for each of the techniques are based on costs from the IAL trials. The costs for a given technique vary between authorities due to the use of different subcontractors, use of internal resources rather than subcontractors, different internal accounting procedures (e.g. different charge rates for staff) and differences in channel and site characteristics (e.g. access, channel width). Where the work can be conducted in-house, the anticipated personnel time required is provided rather than a dollar cost, as this varies from authority to authority, depending on internal charge rates.

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Page last reviewed on 7/3/04