CADDIS Volume 2. Sources, Stressors and Responses: Ionic Strength
On this page:
- Checklist of Sources, Site Evidence and Biological Effects
Ionic strength is the concentration of ionic charge in solution. Increased ionic strength and changes in ionic composition may lead to shifts in community composition and function based on factors such as taxa-specific preferences.
Measurements of electrical conductivity, salinity and total dissolved solids (TDS) are often used to represent the ionic strength of water (see Ways to Measure tab). These measurements generally increase with increasing ion content. This module provides advice for deciding whether or not to include increased ionic strength as a candidate cause of biological impairment.
Because ionic strength issues include a broad range of potential freshwater problems, we are forced to generalize about overall effects. There will be exceptions to these generalizations, especially in terms of taxa-specific reactions to various ion-specific stresses. Nevertheless, this stressor module introduces a common language and identifies some of the more widespread ion-related issues. Ultimately, causal assessors may need to dig deeper into site-specific characteristics and relevant literature.
Ionic compounds are natural constituents of both inland and marine systems. These compounds are not harmful unless levels exceed or fall below the tolerance range of aquatic organisms. Indeed, some constituents of ionic compounds are essential elements, necessary for the survival of aquatic organisms. Salts are ionic compounds composed of cations (positive charge) and anions (negative charge). Common salt ions include:
- Cations: sodium (Na+), calcium (Ca2+), magnesium (Mg2+), potassium (K+)
- Anions: chloride (Cl-), bicarbonate (HCO3-), carbonate (CO32-), sulfate (SO42-)
Ionic strength varies naturally across aquatic ecosystems (Figure 1), and aquatic organisms generally prefer waters with specific ionic strength ranges, containing specific ions. When these parameters are changed, biota may be adversely affected. In recent years, several states (e.g., Florida, West Virginia) have adopted criteria which address the importance of ionic strength in determining water quality.
Ionic strength may significantly impact freshwaters through interactions with other stressors, and it may be difficult to distinguish among proximate stressors and interacting stressors. Potential interactions include:
- Increased salinity may affect the uptake of toxic substances by organisms (Bidwell and Gorrie 2006, Zalizniak et al. 2006, Environment Canada and Health Canada 2001).
- Salts impact soil structure, potentially decreasing soil permeability (Rengassamy 2002), increasing runoff volume and soil erosion (Environment Canada and Health Canada 2001).
- Salt solubility increases as temperature increases.
Salinity, along with temperature and altitude, also affects the solubility of oxygen in water. Freshwater (salinity generally < 0.5 parts per thousand) at 22°C and sea level can hold approximately 8.7 milligrams per liter (mg/L) of dissolved oxygen (DO). Ocean water (salinity ≈ 35 parts per thousand) can hold only about 7.1 mg/L of DO at saturation.
DO saturation might change by 6% over a 10 parts per thousand difference in salinity. With freshwater ecosystems generally falling below 0.5 parts per thousand, the associated DO change over the spectrum of freshwater salinity levels is negligible (Stickney 1979).
This module addresses ionic strength as a proximate stressor. The concentration of hydrogen ions (pH) and heavy metal ions (e.g., lead and zinc), while related to ionic strength and composition, are discussed in separate modules.
Ionic strength should be a candidate cause when human sources and activities, site observations or biological effects support portions of the source-to-impairment pathways (Figure 2). This diagram and some of the other information also may be useful in Step 3: Evaluate Data from the Case.
The checklist below will help you identify key data and information useful for determining whether to include ionic strength among your candidate causes. The list is intended to guide you in collecting evidence to support, weaken or eliminate ionic strength as a candidate cause. For more information on specific entries, go to the When to List tab.
Sources and Activities
- Road salt
- Land cover alteration, leading to dryland salinity
- Water withdrawal
- Combustion wastes
- Resource exploration and extraction (i.e., mining activities)
- Sewage and industrial waste discharges
- Signs of snow disposal
- Crystalline deposits
- Mineral precipitates
- Loss of vegetation
- Presence of salt-tolerant plants
- Decreased productivity of aquatic vegetation
- Unlike other stressors, “rules of thumb” for ionic strength are not listed here. See the When to List tab for common examples of potential biological effects due to changes in ionic strength.
- Flow alteration
- Unspecified toxic chemicals
On this page:
- Sources and Activities that Suggest Listing Ionic Strength as a Candidate Cause
- Site Evidence that Suggests Listing Ionic Strength as a Candidate Cause
- Biological Effects that Suggest Listing Ionic Strength as a Candidate Cause
- Site Evidence that Supports Excluding Ionic Strength as a Candidate Cause
The ionic strength of surface waters is influenced by numerous human activities, in both waterbodies and their associated watersheds. The more extensive the relevant sources and activities, the more likely increased ionic strength will impair surface waters.
Dissolved ions enter waterways from both point and nonpoint sources. Ion transport occurs by overland flow; evaporation and transpiration of water in shallow soil zones, which increases concentrations of dissolved ions; and infiltration through soil into groundwater, with subsequent discharge to lakes, streams and rivers. Increased ionic strength is often positively correlated with watershed urbanization. Watershed surfaces with reduced permeability (e.g., pavement) and storm drain networks transport ions efficiently to surface waters (Roy et al. 2003, Wang and Yin 1997). In addition to ion transport, concentration of ions through evaporation also may influence freshwater ionic strength. For most of the sources listed below, evaporation—due to anthropogenic activities or natural processes—might act as a step in the causal pathway.
Some soil types and geologic formations are natural sources of salts, and certain anthropogenic activities may mobilize and transport those salts to freshwater streams and rivers. Natural geologic variability among neighboring watersheds may result in profound—yet natural—differences in ionic strength of associated streams, especially in arid regions, such as the southwestern U.S. Causal assessors should characterize soil type and geology if ionic strength is being considered as a stressor, particularly if dryland salinity, mining, oil drilling, or irrigation occur in the watershed.
The atmosphere also can be a source of salts to streams and rivers. Rain, snow and wind carry salts to freshwater systems, either in solution or as dry fallout. Along with natural salt sources, the atmosphere may mobilize domestic and industrial pollution with high salt content (Wetzel 2001).
Road salt applied to icy or snowy roads (see Figures 3 and 4), road salt splashed beyond road shoulders, road salt stockpiles, and salt associated with piled waste snow may reach surface waters (Kaushel et al. 2005, Environment Canada and Health Canada 2001, Evans and Frick 2001).
Land cover alteration, such as replacement of native vegetation with shallow root-zone vegetation or vegetation with decreased rainfall interception, can raise water tables and mobilize salts, particularly in regions with naturally saline groundwater, soil or geology. Subsequently, salts may be transported to the ground surface (see Figure 5) or to surface waters via groundwater discharge, a phenomenon sometimes referred to as "dryland salinity" (Rengassamy 2006, National Land and Water Resources Audit 2001).
Water withdrawal for human consumption or irrigation may reduce dilution of dissolved ions in surface waters, thereby increasing ionic concentration. Groundwater withdrawal in coastal areas may cause saltwater intrusion, whereby dissolved ions from marine sources reach otherwise freshwater aquifers. In turn, ions may reach surface waters by mechanisms related to land cover alteration (see above).
Irrigation may mobilize salts by mechanisms similar to the dryland salinity process described earlier. Additionally, irrigation water with high salt content may be introduced to watersheds and reach surface waters by overland flow.
Combustion effluents produced during or mobilized for coal, oil, or wood combustion, including cooling wastewater (blowdown) and ash sluice water, may have elevated ionic content.
Resource exploration and extraction can disturb geologic substrates and mobilize leachable minerals. Improperly cased oil wells may allow mobilization of saline waters (Pond 2004). Waters produced by or used in oil and gas development, mine dewatering, and related activities (e.g., coal bed methane mining; Figure 6), may be saline (Clark et al. 2001).
Sewage and industrial waste discharges often have higher ionic concentrations than receiving freshwaters, as modern wastewater treatment systems are not always equipped to reduce ionic content prior to discharge.
- Signs of snow disposal into or near surface waters
- Crystalline deposits on channel surfaces such as banks, rocks, culverts and drains
- Mineral precipitates appearing as floc, substrate discoloration or cemented organic debris (Figure 7)
- Loss of vegetation including, for example, macrophytes or riparian trees (Williams 2001)
- Presence of salt-tolerant plants such as salt cedar
- Decreased productivity of aquatic vegetation often associated with wilting, bleaching or loss of color and/or stunted growth
There is debate among scientists as to the exact mechanisms responsible for toxicity associated with ionic strength. Toxicity due to ionic strength could result from disruption of organisms' osmotic regulation processes, decreases in bioavailability of essential elements, increases in availability of heavy metal ions, increases in particularly harmful ions, changes in ionic composition, absence of chemical constituents that offset impacts of harmful ions, a combination of the above, or other as yet unknown mechanisms.
In some instances (perhaps the majority), increased ionic strength causes shifts in community composition rather than mortality. Thus, specific conductivity, salinity and TDS levels may be associated with biological impairment and yet be below mortality thresholds.
Toxicity due to ionic strength and composition is often site-specific, species-specific and ion-specific. Horrigan et al. (2005, 2007) developed a numerical salinity index based on the presence/absence of salt sensitive and tolerant macroinvertebrate families.Additionally, Table 1 (below) lists examples of potential biological effects due to changes in ionic strength.
These examples do not apply to all situations. Rather, they provide examples of what causal assessors may find in site-specific biological monitoring data and the type of information that might be found in the literature. Organisms listed in the table are primarily macroinvertebrates. Note that exceptions may exist for many of the summary statements listed below. For example, some amphipods may benefit from slightly increased levels of salinity, but this would depend on ionic composition and the specific taxa present. Before using these generalizations in specific causal assessment tasks, be sure to become familiar with the context of each study.
|Caecidotea and Tipula||Presence associated with elevated conductivity typical of agricultural and urbanized areas (Black et al. 2004)|
|Ceratopogonidae and Tipulidae||Presence in spring-fed surface waters associated with elevated chloride levels attributed to road salt application (Williams et al. 1997)|
|Chlorophyta||Green filamentous alga Cladophora glomerata reported to have affinity for calcium cations (Sikes 1978)|
|Ephemerellidae and Perlidae||Dominance associated with low conductivity typical of forested sites (Black et al. 2004)|
|Gammarus pseudolimnaeus and Turbellaria||Presence in spring-fed surface waters associated with low chloride levels (Williams et al. 1997)|
|Halophilic diatoms||Some diatoms (e.g., Entomoneis) observed to increase with elevated salinity|
|Macrocrustaceans||Amphipods, decapods and isopods (see Figure 8) with high acute lethal salinity tolerance relative to other freshwater taxa (Kefford et al. 2003); amphipods with optima at elevated conductivity levels (Black et al. 2004)|
|Mayflies||Ephemeroptera declined along gradient of increasing conductivity (Pond 2004); some baetid mayflies with low acute lethal salinity tolerance relative to other freshwater taxa (Hassell et al. 2006, Kefford et al. 2003)|
|Orthocladiinae midges (brine- or shoreflies)||Increased with ionic strength in multiple U.S. datasets|
|Soft-bodied non-arthropods||Non-arthropod freshwater macroinvertebrates with soft-bodies (certain Oligochaeta, Gastropoda, Nematomorpha, Tricladida, and Hirudinea) with lower acute lethal salinity tolerance than other freshwater taxa, potentially due to increased permeability to dissolved ions (Kefford et al. 2003)|
There are no site observations that specifically provide evidence of the absence of changes in ionic composition. General reasons for excluding a candidate cause from the list are described in Step 2 of the Step-by-Step Guide and in Tips for Listing Candidate Causes.
We strongly caution against using effects benchmarks (e.g., water quality criteria) as evidence for excluding ionic strength from your initial list of candidate causes. This is because different species have different ionic strength requirements, and different sites have different naturally occurring levels of ionic strength.
Ionic strength is a function of concentration and charge of all ions in a given solution (see Equation 1). Direct measurement of ionic strength is seldom used in ecological studies. Causal assessors are more likely to have access to measures which generally correlate with ionic strength.
- Salinity: Salt content of water (measured in mg/L, grams per liter (g/L), or parts per thousand); parts per thousand can be interpreted as salt mass per 1000 units of water mass, or grams of salt per 1000 grams of water.
- Total dissolved solids (TDS): Concentration of material dissolved in water (measured in mg/L, g/L, or parts per thousand).
Conductivity, salinity and TDS do not fully account for variance in toxicity due to individual ions or ionic composition [refer to Mount et al. (1987) for more information on individual ions and related toxicity], especially for sub-lethal endpoints (Zalizniak et al. 2006). Different solutions with the same ionic strength, conductivity, salinity and TDS may have different effective toxicities, specific to different organisms, if ionic compositions vary. Nevertheless, conductivity, salinity, and TDS may be useful measures of ionic strength, especially in the context of acute toxicity.
In some cases, it may be appropriate to use evidence regarding individual ions (e.g., chloride) if measurements are available and reliable for a particular study site, if the individual ion is a potential causal agent (i.e., concentrations of other ions are low relative to their toxicities), or if regional information describes potential biological effects as a function of exposure to that specific ion.
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Conceptual diagrams are used to describe hypothesized relationships among sources, stressors and biotic responses within aquatic systems.
Geologic and natural sources of ions, in combination with human activities (e.g., agricultural, resource extraction and industrial practices), can contribute to changes in the ion content of streams and rivers. Human activities can increase ionic strength either directly (i.e., introducing new ions) or indirectly (i.e., decreasing ion uptake in watershed, increasing ion delivery to freshwater systems).
For example, industrial, residential and commercial activities may lead to direct discharges of ion-rich waters to surface water, via industrial or wastewater treatment plant effluents. These activities also are associated with increased impervious surfaces, which can lead to increased ion delivery to surface waters.
Direct and indirect pathways (see Figure 9) both may result in increased ion content of surface runoff, subsurface waters, or particles, and ultimately change the ion content of streams and rivers. Groundwater withdrawals near coastal areas may increase the ion content of subsurface water through saltwater intrusion. Activities that increase ion-rich groundwater inputs to freshwater systems (e.g., irrigation) also may change the ion content of receiving waters.
Ion content is related to several other potential stressors, including temperature, sediment, pH, metals, other toxic chemicals and flow alteration. For example, bioavailability of toxic metals can vary with ionic strength, and decreases in pH affect total ionic strength and ionic composition. These potential interactions among stressors should be considered when ionic strength is a possible cause of impairment.
Changes in ions within freshwater systems may affect biota via changes in total ionic strength or ionic composition. Although ionic strength may decrease due to human influences (e.g., downstream of dilute industrial discharges), most often it rises with human activity.
Elevated ionic strength, or large fluctuations in ionic strength over relatively short time periods, may affect freshwater biota via several mechanisms, including increased osmotic stress and increased competition for gill binding sites. For example, changes in ionic composition may adversely impact biota toxic ions become more abundant.
Changes in ionic strength and composition may benefit some aquatic organisms while harming others, ultimately changing organism community composition. This conceptual diagram (See Figure 10) illustrates linkages between ionic strength-related stressors (middle of diagram), the human activities and sources that can affect those stressors (top of diagram), and the biological responses that can result (bottom of diagram).
In some cases, additional steps leading from sources to stressors, modes of action leading from stressors to responses, and other modifying factors also are shown. This narrative generally follows the diagram top to bottom, left to right.
Linking Sources to Proximate Stressors
A number of common sources and human activities may contribute to ionic strength as a proximate stressor, broadly defined as increased total ionic strength or altered ionic composition. Contributing landscape changes (e.g., channel alteration and water withdrawal), natural geologic characteristics, and human activities generally work in combination to effect changes in ionic strength and composition of surface waters.
Most sources are associated with release of wastes from agricultural, resource exploration and extraction, residential, commercial, industrial, and recreational practices. Sources that may have elevated ion content or potentially toxic ionic components include animal wastes, fertilizers, combustion by-products (e.g., cooling water), landfill and septic leachates, road salts and deicing agents, industrial and waste water treatment plant effluents, and mining wastes (e.g., tailings and co-produced water from oil drilling and coal bed methane mining processes).
These waste products may increase ions in subsurface waters, ions adsorbed to particles, and ions in watershed runoff, all of which may ultimately reach surface waters; they also may be discharged directly to streams and rivers. For example, winter safety activities may involve salting paved surfaces and then plowing ion-rich snow into riparian areas, where it melts and carries ions to surface waters.
Human activities may be associated with releases of ion-rich wastes, as described above, or land cover alterations that indirectly alter ionic strength and composition. For example, changes in vegetation or increases in impervious surfaces can increase delivery of ions to streams, via increased deposition and surface runoff. Decreased watershed vegetation may lead to increased soil and bank erosion and decreased nutrient uptake. These impacts may result in increased ion delivery to surface waters via runoff, sediment particles, or subsurface flows.
In addition, mining and other land clearing activities may expose geologic substrates, providing another terrestrial source of ions for surface waters. Groundwater withdrawal in coastal regions may increase the ion content of subsurface water due to saltwater intrusion. Agricultural practices such as planting shallow-rooted vegetation and irrigating crops may raise groundwater table elevations, thereby mobilizing ions which may reach surface waters; this process is sometimes referred to as “dryland salinity.”
Ion content of streams and rivers is related to several other potential stressors, including temperature, sediment, pH, metals, other toxic chemicals, and flow alteration. For example, salt solubility increases as temperature increases; salts can alter soil structure and potentially increase soil erosion (sediment); pH and the bioavailability of toxic substances may vary with ionic strength. Potential interactions among stressors should be considered when ionic strength is a possible cause of impairment.
Linking Proximate Stressors to Biological Impairment
The diagram shows human activities and sources ultimately contributing to two proximate stressors: increases in total ionic strength and changes in ionic composition. Although ionic strength may decrease due to human influences in certain cases (e.g., downstream of dilute industrial discharges), ionic strength most often tends to increase with human activity.
Even though organisms may be capable of handling gradual increases in ionic strength, rapid fluctuations may be harmful and are considered an additional proximate stressor under increased ionic strength.
There is debate among scientists as to the exact mechanisms responsible for toxicity associated with ionic strength, but evidence appears to indicate that elevated ionic strength, or large fluctuations in ionic strength over relatively short time periods, may affect freshwater biota via several modes of action including osmotic stress, increased competition for gill binding sites, and increased ion exchange.
Documented biological responses to ionic strength-related proximate stressors include increased abundance of certain brackish, saltwater, or ion-tolerant taxa (including amphipods, decapods, and isopods) and decreased abundance of certain ion-sensitive taxa such as mayflies and soft-bodied organisms. However, biological responses frequently are site- and species-specific and do not apply to all situations.
Common mechanisms by which changes in ionic composition may adversely impact biota include increased concentration of toxic ions or changes in the toxicity of specific ions. These compositional changes have been associated with decreased bioavailability of essential elements (e.g., magnesium) and with changes in biotic assemblages.
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