3 Post-tsunami assessment and restoration of soil and water
Although there may be visual signs of soil salinity, the most commonly used method to estimate soil salt content is to measure the electrical conductivity (EC) of a soil solution in the laboratory. Soil salinity can also be measured in the field using a portable salinity meter or by assessing the apparent EC (ECa) using an electromagnetic induction soil conductivity meter, such as an EM38 or EM31 instrument.
Salinity assessment methods
Visual indicators of soil salinity (Figure 7) include patchy plant growth; bare soil; salt crystals on the soil surface; puffy, dry soils; and appearance of salt-tolerant plant species. However, if the soil has been cultivated, there may be no visual indicators of the degree of soil salinity.
Laboratory methods to assess soil salinity involve measuring the EC of water extracts of soil samples using either a mixture of one part of soil to five parts of deionised water (EC1:5) or saturated paste (ECe). Different ratios of soil to water may also be used. Care must be taken when interpreting laboratory data because the different ratios of soil to water will give different results. The ratio used by the laboratory should be specified in the results.
Portable salinity meter
Soil salinity can be measured directly in the field by mixing dried, crushed soil with five parts of rainwater, shaking, allowing the mixture to settle, and then measuring the water with a portable (field) salinity meter.
Electromagnetic induction method
Soil EC can be assessed indirectly using electromagnetic induction instruments such as an EM38 or EM31. The EM38 instrument (Slavich et al. 2006a) measures the average ECa of the soil in situ to a depth of approximately 1 m. EM38 surveys are a fast and reasonably accurate method of determining bulk soil salinity levels in the field, particularly across large areas. Measurements across 23 sites in Aceh showed a high correlation between ECa values obtained from using the EM38 and EC1:5 values, to a depth of 40 cm. Given the high variability of soils in tsunami-affected areas, this provides a high degree of confidence in salinity assessments using the EM38 survey method.
ECa readings obtained using the EM38 instrument are influenced by clay content (texture), moisture content, and the presence of metals around the site or on the operator. Using raw figures from an EM38 survey as the basis for salinity action can be misleading, so training is needed in interpreting the results.
EM38 surveys can be used to:
- classify soil salinity risk as low, medium or high
- evaluate the effects of salinity on crop production
- monitor the extent of salt leaching through the soil profile
- identify locations suitable for sampling saline soils for laboratory analysis
- provide a guide to the level of salinity of different texture classes of soils.
Both EC1:5 and ECa can be converted to the EC of a saturated soil (ECe) using a site-specific calibration and a conversion factor based on soil texture (Rhoades et al. 1989; Slavich and Petterson 1993). ECe provides the most reliable measure of salinity for making comparisons between different soil types. Soils are considered saline when the ECe is greater than 2 dS/m.
Monitoring tsunami-affected soils is necessary to assess salinity levels and the rate of leaching, to determine the productive capacity of soils. After the Aceh tsunami, salinity monitoring under the Australian Centre for International Agricultural Research (ACIAR) projects provided information about:
- the impact of the tsunami on crops and yields
- movement of salt through the soil profile
- the rate of return to pre-tsunami conditions.
Box 2 Protocols for using an EM38 instrument to monitor soil salinity
EM38 surveys were very useful in rapid assessment of salinity in Aceh. They showed that the effect of the tsunami on soil salinity was highly variable from one site to another and within a site. Therefore, protocols need to be developed and followed to ensure that readings are taken from representative locations, are reliable and are comparable over time (Slavich et al. 2006a, b). The steps below were used as a standard guide in Aceh:
- Identify sites for surveys based on guidance from local farmers.
- Identify areas of good, medium and poor crop growth, and establish representative sampling transects for each area.
- If more than one soil type is identified, treat each soil type separately, and identify areas of good, medium and poor crop growth on each soil type.
- Determine the start and end of each transect, clearly identify or mark its extent, and record the location and/or the GPS coordinates to enable transect monitoring over time.
- Establish the frequency with which measurements will be taken. This could be a regular interval (e.g. monthly or 3-monthly), after significant rainfall events, or before crop planting and after harvest.
- Follow the instructions for using the EM38 instrument and conduct site-specific calibration using the methods described in Slavich and Petterson (1990).
- Remove metal jewellery and footwear containing metal to avoid affecting the EM38 readings.
- Record visual site conditions at every survey date. Records could include crop stage, recent cultivation, and conditions of the soil surface or crop. Record anything that may affect EM38 readings.
- Record readings in both the vertical (EMv) and horizontal (EMh) orientation at each transect measurement point on each measurement date.
- In flooded sites, measure the depth of water above the soil surface. The height of the instrument held above the surface of the water should be recorded and consistently used between sites and over time. This is needed to enable interpretation of the results—EMh is sensitive to height above ground (EMv is less sensitive).
- Determine the random error of EM38 readings by taking one reading across a full transect and repeating it four times, and then calculating the standard errors of the means. Do this under the three different conditions shown in the photographs: dry soil surface, saturated soil surface and standing water (flooded). This exercise only needs to be done once. It will ensure more accurate interpretation of the site survey data over time.
- Do spot EM38 checks in areas with low growth or yield potential, to identify crop losses that are related to salinity.
- Treat transect locations with very different EM38 readings separately. This will build up the dataset, and enable interpretation of EM38 survey results over time, particularly in relation to movement of salt through the profiles. The ideal time to do this is at the end of the wet season or at the end of harvest.
- Take soil water levels into account when interpreting data. Increased EM38 values during the wet season could be due to increased soil water content.
- Manage EM38 data through project leaders to ensure that only interpreted data are published.
Field observations in Aceh
Changes in field soil salinity between August 2005 and December 2007 were monitored on 23 sites across Aceh Besar, Pidie, Bireuen and Pidie Jaya districts by measuring ECa using an EM38 instrument. ECa values were calibrated using measured EC1:5 data obtained from samples across these sites, and converted to ECe using a factor of 8.6 (Slavich and Petterson 1993), which represents the dominant soil in Aceh’s lowland agricultural areas. The ECa readings in both vertical (EMv) and horizontal (EMh) dipole orientations were recorded during each measurement to allow assessment of both the level of soil salinity and the direction of salt movement.
Monitoring soil salinity using an EM38 instrument (see above, under ‘Field assessment’) helped local agricultural extension agencies identify sites that were too saline for crops and determine when they were suitable for cropping again. This technique can be used following a storm surge or tsunami that leads to agricultural areas being inundated with sea water.
Seawater inundation after the tsunami introduced salinity into areas where it had never been a problem. Eight months after the tsunami, ECe values at the 23 sites varied from 1.6 to 22.6 dS/m (McLeod et al. 2010). Rainfall soon leached salt from most sandy soils. However, clay soils that were inundated for 1–3 days after the tsunami had low to moderate salinity 8 months later, and soils that were inundated for 6 days had higher salinity levels.
Salinity was a significant constraint to crop production during the dry season, and many farmers and extension workers reported declines in yield of around 50%. Three years after the tsunami, ECe values at the same sites ranged from 1.4 to 13.0 dS/m, even though 3,000–7,000 mm of rain had fallen during that period. Likely reasons for the slow leaching of salt are the loss of functional drainage systems and the generally low relief of the affected areas. Salinity tended to be higher in rice paddies that had compacted subsoils, which trapped saline tsunami sediments and held saline water for longer. Salinity also persisted in poorly drained, low-lying areas; in these areas, salinity fluctuated with the seasons. Salts slowly leached from the soil by both vertical displacement through the soil and horizontal movement in surface waters.
A lack of familiarity with soil salinity problems in Aceh resulted in crops being planted in saline soil or irrigated with saline groundwater. This led to failed crops and despair in farmers who were already traumatised by the tsunami. Timely assessments of salinity can help farmers avoid growing crops in saline areas and indicate when management practices are needed to alleviate salinity.
Factors affecting salinity levels after the tsunami
Table 1 presents salinity risk factors for crop production after the tsunami, based on information collected from local farmers and field extension officers during site visits and EM38 surveys in Aceh’s eastern districts. Some of these risk factors are discussed below.
Risk of soil salinity affecting crop production
Duration of inundation with sea water
Less than 0.5 days
More than 3 days
Low (e.g. puddled clays with shallow watertable)
Moderate (e.g. non-puddled loamy soils)
High (e.g. sandy soils)
Inundation by tidal water
Information not available
Tidal water only moderately saline
Irregularly covered by tidal water of high salinity
Number of irrigated rice crops since the tsunami
Information not available for more than two rice crops
Depth and salinity of shallow watertable
No data, but likely to be low risk if below 2 m in dry season and EC < 2 dS/m
No data, but likely to be medium risk if 1–2 m from surface in dry season and EC = 2–4 dS/m
Less than 1 m from surface in dry season, and EC > 4 dS/m
EC = electrical conductivity
Source: Slavich et al. (2006a)
Duration of seawater inundation
The length of seawater inundation after the tsunami determined the level of salinity risk for crop production. Highest salinity levels occurred where sea water stayed on the soil for weeks after the tsunami, allowing salts to penetrate the soil and attach to clay particles. Land inundated for more than 3 days was usually too saline for most crops to yield well in the first 12 months (Table 1).
Soil texture plays a crucial role in soil salinity. The level of clay in soils can be estimated using hand texture tests in the field, or measured using the standard particle size analysis method in the laboratory. In the hand texture test, a handful of soil is mixed with water to form a small ball about 2 cm in diameter. The ball is then pressed between fingers and thumb to form a ribbon; the longer the ribbon, the more clay is in the soil.
Sandy soils tended to be less saline after the tsunami because salts do not attach to sand particles and so are easily leached through the soils. Peat soils also leached salt relatively quickly through surface drainage networks. Clay soils drain more slowly than sandy or peat soils, and salts tend to attach to clay particles, so clay soils remained saline for longer. In heavy clay soils around Bireuen on the east coast of Aceh, where rainfall is relatively low (~1,600 mm/year), salinity persisted for more than 12 months, reducing crop yields. In poorly drained soils, salts are mainly lost via surface flow of water rather than by leaching through deeper layers (Nakaya et al. 2010).
Sandy sediments leached salts easily, whereas clay sediments held salts more tightly. The organic matter in peaty sediments tended to buffer the salt concentration so that the salt did not affect plant growth. However, the underlying soil type is more important than sediment type for predicting soil salinity levels. If the soil underneath the sediment is sandy, leaching will occur; if it is clay, the salts will tend to remain, even if the sediment is sandy.
Availability of fresh water for leaching salt from the soil
Sea water is more likely to infiltrate dry soils than wet soils. When assessing soil salinity after seawater inundation, knowledge about rainfall just before the tsunami will provide information on the soil moisture conditions and therefore the likelihood of infiltration by sea water. Knowledge about rainfall after the tsunami will provide information on the likelihood of salt leaching after the event.
Although no rainfall data for Aceh were available before the tsunami, it is likely that the soil was wet because the tsunami occurred during the wet season (the rice-growing season). At sites with similar rates of drainage, the leaching of salts from the soil profile is principally affected by the annual rainfall. The higher the rainfall, the faster salt is leached out. The average rainfall on the west coast of Aceh is 2,300–3,300 mm/year, compared with 1,365–1,889 mm/year on the east coast. It is likely that greater salinity occurred on the east coast than the west coast because of the slower rate of leaching.
Rice soils are compacted and clay based to hold water. As a result, they do not leach salts vertically, and required flushing with rainfall or irrigation after the tsunami to remove salt laterally. Lower salinity levels were observed in areas where there was plenty of fresh water for irrigation and flushing. Rainfed paddy fields were more likely to be saline for longer because the salts could not be flushed away until the wet season. In some areas, the tsunami increased salinity levels in well water and groundwater, which meant that irrigation added additional salt to the soil.
Soil tended to be more saline in the centre of the rice paddies than in the outer sections, because the centre section was often a drainage basin for the rest of the site and difficult to flush out. Through-flow of surface water is particularly important when establishing rice on tsunami-affected land.
In Sri Lanka, upland fields and home gardens relied on rainfall to remove salt from the soil. Finding methods to flush salt from soils in low-rainfall zones was important for restoring productive home gardens (Weligamage et al. 2005). Rehabilitation of ponds and other water storages was vital to collect irrigation water to leach salts from field soils.
The research of Nakaya et al. (2010) in upland fields and plantations of Thailand proposed a method to calculate the amount of water needed to remove salt from soil with poor drainage. If farmers were provided with rainfall gauges, and trained in measuring and recording rainfall, they could learn to correlate rainfall with the rate of return of healthy crops. Combined with the removal of highly saline sediment and construction of shallow drains to facilitate salt leaching, this method could easily be converted into an extension package for advisers to help farmers determine when salinity risk has dropped to an acceptable level.
In Aceh, sites selected for monitoring had all been inundated by sea water. They covered a range of soil types and were located in different agricultural areas of the province. Background information was gathered for each site to make sense of monitoring results; this involved answering the following questions:
- How long did sea water cover the site?
- What type of sediment was left behind?
- How deep was the sediment?
- How was the sediment treated?
- Was topsoil eroded and, if so, to what depth?
- Is the site now affected by tidal water?
- Is there good drainage at the site?
- Is the site dryland or irrigated?
- Is fresh irrigation water available?
- Are there problems with irrigation or drainage at the site?
- Before the tsunami, what crops were grown and what were their yields?
- What is the cropping history and yield since the tsunami?
- Does the site have any other special characteristics?
The ACIAR projects in Aceh monitored 23 permanent sites every 3 months for:
- soil salinity
- soil texture (salt movement differs in clay and sandy soils)
- depth of water above the ground at flooded sites (this is important when interpreting EM38 salinity readings)
- soil nutrients (nitrogen, phosphorus, potassium, organic matter)
- soil pH
- salinity and pH of surface water and well water
- crop performance in the ground (leaf appearance, grain or fruit appearance, potential yield, yield).
Sampling protocols for soil, water and crops
Projects in Aceh adopted the following protocols for sampling:
- Assign and clarify responsibilities for sampling, analysing soil and plant samples, and analysing and interpreting data.
- Train field technical staff to collect and process soil samples. In Aceh, the field technical staff were from the Assessment Institute for Agricultural Technology (BPTP) Aceh.
- Take one soil profile at each site to a depth of at least 60 cm, with samples divided into 0–20 cm, 20–40 cm and 40–60 cm depths. Keep each sample in a bag that is clearly labelled to show location, date and depth of sample. Samples should be air dried and ground to pass through a 2mm sieve before they are sent to the designated soil laboratory for analysis. The soil laboratories in BPTP Aceh and the Indonesian Soil Research Institute (ISRI), Bogor, were the designated laboratories for soil chemical analyses.
- Sample well water and surface water at each soil and crop assessment site, whenever possible. Record the sample depth and field EC. Submit well water samples to the laboratory to confirm the EC and pH. Note the water colour, particularly indicators of soluble iron after storage (oily surface and yellowing).
- Monitor the EC1:5 at selected points in the trial area. This should be done without combining samples, because soil EC is spatially variable. Sampling points could be based on visual indicators of plant growth (e.g. poor, medium and good growth).
- Take plant tissue samples where there is evidence of crop nutrition or soil fertility problems.
Records of soil and water measurements at each trial site—including a dedicated field diary of EM38 survey measurements—showed salt movement over time, and built a database of post-tsunami soil recovery. Notes on crop growth and performance at each site helped to determine whether salinity was an issue.
The ACIAR projects in Aceh developed several strategies, described below, to help advisers and farmers deal with salinity.
Leaching and flushing of salt from soil
Aceh’s naturally high rainfall encouraged leaching of salts down through the soil profile, especially in sandy soils (Slavich et al. 2006b). Leaching of saline sites can be encouraged by:
- raising crop beds to improve drainage (see below)
- constructing shallow drainage channels to encourage surface flushing of salt during rainfall
- mulching beds to prevent soil from drying out and bringing salts to the surface.
Flushing fields using irrigation water and natural rainfall is possible once drainage and irrigation channels are cleared of sediment and a through-flow of water is available. Pumps might be needed to remove saline water in low-lying areas. In Aceh, salt in rice soils was close to the ground surface because the soils were already flooded, and the compacted, puddled soils prevented the salt from leaching down through the soil. Where farmers had access to irrigation water and drainage was unimpeded, this surface salt was easily flushed away. Rice crops appeared unaffected by the tsunami 7 months later, even where tsunami deposits were present.
Farmers in rainfed fields may need to wait longer for salts to be leached from the soil if no local source of irrigation water is available. Nakaya et al. (2010) proposed a method in Thailand to predict the long-term impacts of salt, based on climatic conditions, and calculated the water requirements to mitigate soil salinity in rainfed farming systems. Their findings supported other observations (Raja et al. 2009) that salinity decreased with increasing rainfall, and only a shallow layer of surface soil may need to be removed initially to reduce salt levels in the short term.
Soil salinity at depth can remain an issue for longer, depending on the local hydrology and the extent of saline water intrusion into groundwater. This type of salinity may affect deep-rooted crops and tree crops. Studies in Thailand and Aceh (Nakaya et al. 2010; Marohn et al. 2012) observed long-term impacts from saline groundwater on mortality and yields of common tree crops in coastal areas.
Removal of saline water
Where poor drainage or post-tsunami damage impedes the flushing of salt-affected fields with fresh water, the removal of saline water with pumps is an option. In 2005 in the district of Pidie, rice in one bunded field failed, while crops in bunded fields on either side grew normally (Figure 8). The difference in management was that some farmers could afford to pump saline water from their fields, reducing the salinity levels at planting, and establish crops before the start of the wet season, whereas the owner of the failed crop waited for rain to plant. At the time the photo was taken, surface water EC readings were low (~0.2 dS/m) in both fields; however, they were probably higher in the failed crop at planting because no removal or flushing of surface salts was possible.
Use of raised beds
Raised crop beds allow water to drain quickly from the soil, taking any salt with it. This is a useful technique in high-rainfall areas, but not as useful during dry periods when the demand for water is high. On more elevated sites, the construction of shallow drainage channels will help to leach salt from soils.
Use of calcium
Adding calcium to saline soils replaces sodium, effectively leaching the sodium from the soil. Calcium is commonly added in the form of gypsum. Where gypsum is unavailable, poultry manure, which is high in calcium, could be used. These options were rarely used in Aceh, mainly because of the high cost of gypsum and a scarcity of poultry manure.