What is bore water?
Bore water is groundwater that has been accessed by drilling a bore into underground water storages called aquifers. An aquifer is formed when water from rain and rivers seeps through layers of soil and rock and fills spaces or fractures within layers of sand and fractured rock.
Bore water may be suitable for uses including stock watering, irrigation, flushing toilets and washing clothes or cars. It may even be suitable for showering, food preparation and drinking. However, bore water can become contaminated by natural processes and human activities. Testing by an accredited laboratory is required to confirm the quality of the water, which may require treatment, depending on its intended use.
If your bore water is required for human consumption, you should have it tested at least once a year for chemical content and microbiological contamination. (Please ask for the Vintessential Drinking Water Fact Sheet.)
Is my bore water suitable for watering?
There are two important chemical parameters that should be tested before using bore water – pH and Salinity. Vintessential offers a Bore Water testing bundle for $33 (including GST) per sample.
Measurement of pH is one of the most important and frequently used tests in water chemistry. It indicates if the water is alkaline (pH>7), neutral (7) or acid (<7). For irrigation purposes, pH 5.5 to 8.5 is suitable for most plants.
Salinity indicates the amount of dissolved salts expressed as mg/L (milligrams per litre). Different plants can tolerate different levels of salinity in water, but can also be influenced by soil type and characteristics.
Bore water that is very acidic can be highly corrosive, whilst if it is highly alkaline (hardness caused by calcium and magnesium salts), crusts may form on bore pipes and fittings. Salinity measuring more than 1000mg/L may cause scaling and corrosion on bore pipes and fittings and leaf burn on plants.
Collecting your water sample
- If not using the sample bottle provided by Vintessential, ensure that your collecting container is veryclean and dry.
- Choose a sample which is representative of the body of water being considered. It needs to be asample which is most like the water you want to get information about. Try not to take your sample tooclose to the surface, bottom or sides of the water source.
- Bores can be tested at the trough. However, the water should be freshly pumped. The salinity of watersitting in an unused trough may be higher than the actual groundwater salinity level due to concentration of the salts through evaporation.
- Rinse the container two or three times with some of the water to be sampled.
- Collect the sample and fill container completely so there is no air pocket.
- Secure the lid firmly and deliver to laboratory ASAP.
- Do not freeze or allow the sample to become too warm.
Easy Test Sampling Packs
To assist you to collect your water samples, pick up a FREE Easy Test Sampling Pack from your nearest laboratory.
The Easy Test Pack provides:
- Sample container
|Salinity Range (mg/L)
|Guide to Usefulness for Irrigation
|Generally good for irrigation
|Consider tolerance of plants, soil type, ensure good drainage
|Not normally suitable for irrigation, only use for very tolerant plants
|Not suitable for irrigation
The following table provides an indication of the salinity tolerance of groups of plants:
Range of salinity of natural waters shown below:
|35000 – 40000 mg/L
|3 – 60 mg/L
|Fresh water lake
|20 – 1000 mg/L
|Fresh underground water
|100 – 1000 mg/L
|Saline underground water
|1000 – 350000 mg/L
(Note – The division between fresh and saline water is arbitrarily taken as 1000mg/L)
Garden Plants Maximum Recommended Salinity (mg/L)
The following table is a guide to the salt tolerance of various garden plants, growing under average conditions of soil types and drainage:
|700 – 1500 mg/L
|1500 3000 mg/L
Avoid wetting leaves in hot, dry days
Avoid light, frequent watering and wetting leaves during daytime
Australian Native species
Avoid wetting leaves
Download the Bore Water Test Bundle Factsheet
© Vintessential Laboratories 2016. No part of this publication may be reproduced, stored in a retrieval system or transmitted in any form or by any means without the prior written permission of the publisher.