By: Bonnie L. Grant, Certified Urban Agriculturist
Soil provides sodium in plants. There’s a natural accumulation of sodium in soil from fertilizers, pesticides, run off from shallow salt-laden waters and the breakdown of minerals which releases salt. Let’s learn more about sodium in plants.
What is Sodium?
The first question you need to answer is, what is sodium? Sodium is a mineral that is generally not needed in plants. A few varieties of plants need sodium to help concentrate carbon dioxide, but most plants use only a trace amount to promote metabolism.
So where does all the salt come from? Sodium is found in many minerals and is released when they break down over time. The majority of sodium pockets in soil are from concentrated runoff of pesticides, fertilizers and other soil amendments. Fossil salt runoff is another cause of high salt content in soils. The sodium tolerance of plants is also tested in coastal areas with naturally salty ambient moisture and leaching from shorelines.
Effects of Sodium
The effects of sodium in plants are similar to those of exposure to drought. It’s important to note the sodium tolerance of your plants, especially if you live where groundwater run-off is high or in coastal regions where ocean spray drifts of salt to plants.
The problem with excess salt in soil is the effects of sodium on plants. Too much salt can cause toxicity but more importantly, it reacts on plant tissues just as it does on ours. It produces an effect called osmotion, which causes important water in plant tissues to be diverted. Just as in our bodies, the effect causes tissues to dry out. In plants it can impair their ability to even uptake adequate moisture.
Buildup of sodium in plants causes toxic levels that cause stunted growth and arrested cell development. Sodium in soil is measured by extracting the water in a laboratory, but you can just watch your plant for wilting and reduced growth. In areas prone to dryness and high concentrations of limestone, these signs are likely to indicate a high salt concentration in soil.
Improving Sodium Tolerance of Plants
Sodium in soil that’s not at toxic levels can easily be leached out by flushing the soil with fresh water. This requires applying more water than the plant needs so the excess water leaches away the salt from the root zone.
Another method is called artificial drainage and is combined with leaching. This gives the excess salt laden water a drainage area where water can collect and be disposed of.
In commercial crops, farmers also use a method called managed accumulation. They create pits and drainage areas that funnel salty waters away from tender plant roots. The use of salt tolerant plants is also helpful in managing salty soils. They will gradually uptake sodium and absorb it.
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Read more about Soil, Fixes & Fertilizers
Alkali, or Alkaline, soils are clay soils with high pH (> 8.5), a poor soil structure and a low infiltration capacity. Often they have a hard calcareous layer at 0.5 to 1 metre depth. Alkali soils owe their unfavorable physico-chemical properties mainly to the dominating presence of sodium carbonate, which causes the soil to swell  and difficult to clarify/settle. They derive their name from the alkali metal group of elements, to which sodium belongs, and which can induce basicity. Sometimes these soils are also referred to as alkaline sodic soils.
Alkaline soils are basic, but not all basic soils are alkaline.
Potassium–sodium interactions in soil and plant under saline‐sodic conditions †
Institute of Soil and Environmental Sciences, University of Agriculture, 38040 Faisalabad, Pakistan
Institute of Soil and Environmental Sciences, University of Agriculture, 38040 Faisalabad, PakistanSearch for more papers by this author
Institute of Soil and Environmental Sciences, University of Agriculture, 38040 Faisalabad, Pakistan
Institute of Soil and Environmental Sciences, University of Agriculture, 38040 Faisalabad, PakistanSearch for more papers by this author
This article is based on a talk at the IPI‐ISSAS 12th International Symposium on Management of Potassium in Plant and Soil Systems in China, Chengdu, Sichuan, China, July 25–27, 2012.
About 7% of the total land around the globe is salt‐affected causing a great loss to agriculture. Salt stress refers to the excessive amount of soluble salts in the root zone which induce osmotic stress and ion toxicity in the growing plant. Among toxic ions, sodium (Na + ) has the most adverse effects on plant growth by its detrimental influence on plant metabolism in inhibiting enzyme activities. An optimal potassium (K + ) : Na + ratio is vital to activate enzymatic reactions in the cytoplasm necessary for maintenance of plant growth and yield development. Although most soils have adequate amounts of K + , in many soils available K + has become insufficient because of large amounts of K + removal by high‐yielding crops. This problem is exacerbated under sodic or saline‐sodic soil conditions as a consequence of K + ‐Na + antagonism. Here K + uptake by plants is severely affected by the presence of Na + in the nutrient medium. Due to its similar physicochemical properties, Na + competes with K + in plant uptake specifically through high‐affinity potassium transporters (HKTs) and nonselective cation channels (NSCCs). Membrane depolarization caused by Na + makes it difficult for K + to be taken up by K + inward‐rectifying channels (KIRs) and increases K + leakage from the cell by activating potassium outward‐rectifying channels (KORs). Minimizing Na + uptake and preventing K + losses from the cell may help to maintain a K + : Na + ratio optimum for plant metabolism in the cytoplasm under salt‐stress conditions. It would seem a reasonable assumption therefore that an increase in the concentration of K + in salt‐affected soils may support enhanced K + uptake and reduce Na + influx via HKTs and NCCSs. Although very useful information is available regarding K + ‐Na + homeostasis indicating their antagonistic effect in plants, current knowledge in applied research is still inadequate to recommend application of potassium fertilizers to alleviate Na + stress in plants under sodic and saline‐sodic conditions. Nevertheless some encouraging results regarding alleviation of Na + stress by potassium fertilization provide the motivation for conducting further studies to improve our understanding and perspectives for potassium fertilization in sodic and saline‐sodic environments.
Cooperative Extension: Garden & Yard
Written by Dr. Lois Berg Stack, Extension Professor (2011). Revised by Dr. Lois Berg Stack, Extension Professor, and Mark Hutchinson, Extension Professor (2012). Revised by Dr. Lois Berg Stack, Extension Professor (2016)
Note to readers: This document contains many common soil science terms. Understanding these terms, which are italicized in the text, will help you understand soils as you read gardening books.
Soil is a dynamic three-dimensional substance that covers some of the world’s land surface. It varies from place to place, in response to the five factors that form it: climate, topography, organisms, the parent rock below surface, and time. Our Maine soils developed since the last glacier moved across the region, largely in response to the parent rock (largely granite) and topography. Most Maine soils are acidic, and have a somewhat depressed ability to hold and exchange nutrients used by plants. Our native plants evolved in this system, and are well adapted to Maine soils. However, we often amend Maine soils by adding organic matter, lime and/or fertilizer, in order to increase the productivity of our food and landscape plants.
Soil performs four major functions:
- It provides habitat for fungi, bacteria, insects, burrowing mammals and other organisms
- It recycles raw materials and filters water
- It provides the foundation for engineering projects such as buildings, roads and bridges and
- It is a medium for plant growth. This text focuses on this last function.
What does soil do for plants?
Soil supports plant growth by providing:
- Anchorage: root systems extend outward and/or downward through soil, thereby stabilizing plants.
- Oxygen: the spaces among soil particles contain air that provides oxygen, which living cells (including root cells) use to break down sugars and release the energy needed to live and grow.
- Water: the spaces among soil particles also contain water, which moves upward through plants. This water cools plants as it evaporates off the leaves and other tissues carries essential nutrients into plants helps maintain cell size so that plants don’t wilt and serves as a raw material for photosynthesis, the process by which plants capture light energy and store it in sugars for later use.
- Temperature modification: soil insulates roots from drastic fluctuations in temperature. This is especially important during excessively hot or cold times of year.
- Nutrients: soil supplies nutrients, and also holds the nutrients that we add in the form of fertilizer.
Physical properties of soil
Texture: Soil is composed of both minerals (derived from the rock under the soil or transported through wind or water) and organic matter (from decomposing plants and animals). The mineral portion of soil is identified by its texture. Texture refers to the relative amounts of sand, silt and clay in the soil. These three terms refer only to particle size, not to the type of mineral that comprises them. Sand is familiar to most of us, and is the largest textural soil size. Sand grains can be seen with the naked eye or with a hand lens. Sand provides excellent aeration and drainage. It tills easily and warms up rapidly in spring. However, it erodes easily, and has a low capacity for holding water and nutrients. Clay particles are so small that they can only be seen through an electron microscope. Clay soils contain low amounts of air, and water drains slowly through them. Clay is difficult to till, and warms up slowly in spring. But, it tends to erode less quickly than sand, and it has a high capacity for holding water and nutrients. Silt is sized between sand and clay. Individual silt particles can be seen through a lower-power microscope. It has intermediate characteristics compared to sand and clay.
Most soils contain all three particle sizes (sand, silt, clay). Loam is a term that is often used generally to refer to soils that are a mixture of sand, silt and clay. Most of our topsoils are loams. However, “loam” can vary from a rather equal mixture of the three textural sizes, to a mixture dominated by sand or silt or clay. As a gardener, you should inspect loam before purchasing it, because these variations affect management practices.
Structure: Sand is often found as individual particles in a soil, but silt and clay are almost always clumped into larger units called aggregates. The manner of this aggregation defines a soil’s structure. Soil structure is described by terms such as blocky, platy, prismatic and angular. Productive topsoils often have a granular soil structure. The size and shape of aggregates is influenced by mineral type, particle size, wetting and drying, freeze/thaw cycles, and root and animal activity. Decomposed organic matter, plant sugars excreted from roots, waste products of soil microbes, and added soil conditioners all act to cement particles into aggregates. However, aggregates can break apart from tilling, compaction, and loss of organic matter in the soil. Soil structure is a very dynamic process. Good soil structure increases the pore space (see below) that supports root penetration, water availability and aeration.
Pore space: Soil particles rarely fit together tightly they are separated by spaces called pores. Pores are filled with water and/or air. Just after a heavy rainfall or irrigation event, pore spaces are nearly 100% filled with water. As time goes by, the water passes through the soil due to gravity, or evaporates into the air, or is used by plant roots, and more of the pore spaces are filled by air. Particles of clay fit tightly, and have very little pore space to hold air and water. On the other hand, sand on a beach has such a large amount of large pores that it drains too quickly to grow most plants in.
Pore space generally occupies 30-60% of total soil volume. A well-structured soil has both large pores (macropores) and tiny pores (micropores) this provides a balance of the air and water that plants need. Macropores provide for good drainage, and micropores hold water that plants can access. This helps explain how you can achieve a “well-drained but moist soil”.
Organic matter (OM) is previously living material. On the soil surface, there is usually rather un-decomposed OM known as litter or duff (or, mulch in a landscape). This surface layer reduces the impact of raindrops on the soil structure, prevents erosion, and eventually breaks down to supply nutrients that leach into the soil with rainfall or irrigation. In the soil, OM decomposes further until it becomes humus, a stable and highly decomposed residue. Humus is an important nutrient source for plants, and it is important in aggregating soil particles.
OM is always in the process of decomposing, until it becomes humus. OM levels are reduced through cropping and can be replenished by adding compost or manure, or crop residues, or green manure (crops such as buckwheat, clover or ryegrass that are grown as cover crops and then tilled into the soil). Soil OM can be conserved with reduced tillage practices, such as no-till. OM improves water retention, making it a good addition to sandy soil. OM is also added to clay or silt soils to increase aggregation and thereby improve drainage. OM provides nutrients as it decomposes, buffers the pH of the soil solution (see below) against rapid chemical changes, and improves soils’ cation exchange capacity (see below).
Good horticultural soil: Most soils are dominated by mineral particles some are dominated by organic matter. Some soils have a high percentage by volume of pore space, while others have little pore space. Your soil might vary from one part of your land to another. Ideally, a “good horticultural soil” contains 50% solid material (mostly mineral soil plus 5-10% organic matter) and 50% pore space. At any given time, that pore space is occupied by both air and water. You can assess your soil by irrigating heavily, then allowing it to drain for a day. After a day of drainage, the pore space should contain about 50% water and 50% air. If the soil is very dry after a day of drainage, it is likely dominated by sand, and you could amend it over time by adding OM. If the soil remains very wet, it is likely dominated by clay or it is not well aggregated you could amend such a soil over time by adding OM to support aggregation.
Chemical properties of soil
Soil chemical activity is related to particle size, because chemical reactions take place on particle surfaces. Small particles have much more surface area than large particles. Small soil particles play a big role in two chemistry-related processes: managing soil acidity (pH), and supporting the soil’s ability to hold nutrients (CEC).
First, it’s important to know that fertilizers are salts. When salts dissolve into the soil solution, they separate into a cation (a positively charged ion) and an anion (a negatively charged ion). For example, when we dissolve table salt (sodium chloride) in water, it separates into positively charged sodium and negatively charged chloride ions. When we add sodium nitrate fertilizer to the soil, it dissolves into the soil solution as sodium cations and nitrate anions.
Tiny particles (humus and clay) are very important for holding plant nutrients in the soil. Clay and humus particles have a negative surface charge. Cations are positively charged. Because opposites attract, the clay and humus hold cations, and prevent them from being leached out of the soil by water movement. Negatively charged anions remain dissolved in the soil solution, and are very susceptible to leaching downward.
Nitrogen is an interesting nutrient, because one nitrogen fertilizer might be positively charged ammonium that is held by soil particles, while another nitrogen fertilizer might contain negatively charged nitrates that remain dissolved in the soil solution. This explains why nitrates, which are anions, leach readily out of our topsoil and sometimes into our water supply. It also explains why “slow-release fertilizers” usually contain ammonium, which can be held by the soil particles and gradually converted to the nitrate form that most plants use readily.
Cation exchange capacity (CEC) is an expression of the soil’s ability to hold and exchange cations. Ions are constantly exchanged among the soil solution, CEC sites on clay and humus particles, and plant roots. This is not a random process, but is dependent on electron charge. Clay and humus have high CECs because they are tiny particles with very large surface-to-volume ratio, with many negative sites that can attract cations. Sand has very low CEC because sand particles are large, with low surface-to-volume ratio and hence fewer negative sites. A gardener can add higher rates of fertilizer less frequently when gardening in a soil with a high level of clay or humus, compared to a sandy soil, because cations (potassium, calcium, magnesium and others) are held by soil particles. Because a sandy soil cannot hold the same amount of cations, fertilizing them more frequently with smaller amounts of fertilizer is a better option.
pH: pH is a description of the soil’s acid/alkaline reaction. The pH scale ranges from 0 (very acid) to 14 (very alkaline). Soils generally range from pH 4.0 to pH 8.0. Northeastern forest soils can be very acid (pH 3.5), while Western soils can be very alkaline (pH 9). pH is important because it regulates the availability of individual nutrients in the soil solution.
The pH scale is logarithmic each unit is 10 times more acid or alkaline than the next. For example, a soil with pH 4.0 is ten times more acid than a soil with pH 5.0, and 100 times more acid than a soil with pH 6.0. A soil’s pH depends on the parent rock (limestone is alkaline, granite is acidic), rainfall, plant materials, and other factors. Individual plants perform best within specific pH ranges. It is just as important to manage pH as fertility. Most garden plants perform well in a soil with pH 6.0 – 7.0. Acid-loving plants such as rhododendron and blueberry perform well in a soil with pH below 5.0.
Living organisms in soil
Many organisms inhabit soil: bacteria, fungi, algae, invertebrates (insects, nematodes, slugs, earthworms) and vertebrates (moles, mice, gophers). These organisms play many physical and chemical roles that affect plants. For example, their secretions help dissolve minerals, making them available to plants some organisms convert inorganic substances into other forms that are more or less available to plants organisms add OM to the soil organisms help decompose OM many organisms aerate the soil. Some living organisms in the soil cause diseases, some feed on plant tissue, and many compete with plants for nutrients and water.
Rhizosphere: The very thin zone of soil just around roots is called the rhizosphere. This zone is different from the rest of the soil, and it sometimes supports specific and unique organisms. For example, some fungi live together with roots, to their mutual benefit these mycorrhizal relationships provide the fungi with a place to live, and the fungi assist in the plant’s water and nutrient uptake. Similarly, some nitrogen-fixing bacteria grow together with some plants, including many legumes (members of the bean family). The bacteria convert atmospheric nitrogen into forms that can be used by their host plants. When the host plant dies, the nitrogen compounds released during decomposition are available to the next crop. Any mutually beneficial relationship between two dissimilar organisms is called a symbiosis.
Water is an amazing substance. It is called the universal solvent because it dissolves more substances than any other liquid. It is a renewable natural resource. It exists in nature as a solid, liquid and gas. Its molecules cohere (stick together) and adhere (stick to) to other surfaces this accounts for its ability to reach the top of tall trees. It has a high latent heat, which means that it releases a large burst of energy when it passes from solid to liquid and from liquid to gas. And, when it passes from gas to liquid and from liquid to solid, it absorbs a large burst of energy. Gardeners reap the benefits all of these attributes of water.
Water-holding capacity: A soil’s ability to hold water is called its water-holding capacity. Clayey soils have high water-holding capacity, while sandy soils have low water-holding capacity. As a soil’s pore space is filled with water by heavy rainfall or irrigation, the soil becomes saturated. Then, water gradually drains downward, and the amount of water remaining in the soil against the force of gravity is called the soil’s field capacity. Clayey soils drain much more slowly than sandy soils. Loamy soils reach their field capacity 2-3 days after a heavy rainfall or irrigation. If no more water is added, the soil continues to dry out plants take up some of the water, and some water moves upward in the soil and evaporates from the surface. Eventually, a soil may dry enough to reach its permanent wilting percentage, the point at which a plant wilts so severely that it cannot recover. At this point, the available water (water that remains available to the plant) is gone, and the only water that remains in the soil is so tightly bound to soil particles that plants cannot access it.
It’s important to understand a soil’s water holding capacity so that we can use appropriate irrigation practices. Irrigating a heavy clayey soil and a sandy soil in the same way would result in very different results.
Good soil management is critical for crop productivity. Good management must include consideration of maintaining the soil’s integrity over time. Poor management can lead to erosion, loss of fertility, deterioration of soil structure, and poor crop yields.
Tilling: Mechanical manipulation of soil loosens the soil, and promotes aeration, porosity and water-holding capacity. It allows a gardener to incorporate soil amendments such as OM and lime. On the other hand, tilling tends to decrease aggregation, causing compaction (compacted soils are dominated by few, small pores). It can take years to overcome the damage caused by overtilling.
Managing pH: Soil pH regulates the availability of plant nutrients. pH should be managed only in response to soil test results. Soil pH can be lowered by adding some kinds of organic matter or sulfur or sulfates this is not often needed in Maine soils. Soil pH can be raised by adding lime or some types of fertilizer or wood ash. It is difficult to overcome the negative effects of applying excessive amounts of these materials. Test first!
Mulching: Mulch is a material that covers the soil. Organic mulches such as compost, aged manure or bark chips decompose to supply OM and nutrients in the long term. Inorganic mulches such as stone or plastic sheet materials have little effect on nutrient levels and do not contribute OM to the soil. All mulches affect soil temperature by insulating or transferring heat, and all mulches help soils retain moisture. Mulches may also help reduce weed growth, prevent erosion and affect insect/disease presence.
Managing OM levels: In natural areas, plants and animals die, decompose and replenish OM in the soil. Each year, plant leaves deciduate and rot (compost) in place, and their nutrients and OM are added to the soil through rainfall and the freeze/thaw cycle that creates cracks in the soil. On the other hand, in developed landscapes where this natural cycle is interrupted, gardeners must implement processes to replenish soil OM. Leaves from deciduous trees can be left in place to decompose plant debris can be composted and incorporated back into gardens as OM and plant residue, green manures and animal manures can be incorporated directly into the soil. Some tillage is generally required to incorporate this material into the soil. Adding huge amounts of OM at one time can cause nutrient problems, especially if the material is not fully composted. Adding small amounts of OM periodically can contribute to longterm soil fertility, support soil microflora, contribute to good soil structure, and support the soil’s ability to hold both water and air.
Three elements, carbon, oxygen and hydrogen, are essential to plant growth and are supplied by air and water. The other essential elements are referred to as plant nutrients, and are provided by the soil, or are added as fertilizers, and enter plants almost exclusively through the roots. These plant nutrients are divided into two groups. Those required by plants in large amounts are called macronutrients these are nitrogen, phosphorus, potassium, calcium, magnesium and sulfur. Plant micronutrients, needed in tiny amounts include iron, chlorine, zinc, molybdenum, boron, manganese, copper, sodium and cobalt. Macronutrients and micronutrients are all critical to normal plant growth and development they are simply needed in different amounts.
Organic fertilizer sources include compost, aged manure, rock phosphate, soybean meal, and fish meal. Organic fertilizer can also be “grown” by planting a legume cover crop, which is a crop that is grown with the intention of tilling it into the soil, at which point it is referred to as a green manure. Cover crops also add OM to the soil. Inorganic fertilizer products are also widely available, either as single-nutrient or multi-nutrient products.
Fertilizers are labeled as slow-release or soluble. Slow-release fertilizers provide nutrients over a period of time, as they break down or decompose. Soluble fertilizers are fast-release, and many are dissolved into water and then irrigated onto crops.
Nutrients can be provided by many products and practices. Price, availability, ease of use, needed equipment, time and philosophy should be considered when selecting the best fertilizer and application method for any situation. Occasionally, in severe nutrient deficiency situations, some micronutrients are sprayed onto the foliage of crops, but most are applied to the soil and taken up by roots. In hydroponic production systems, nutrients are dissolved in water and washed over the exposed roots of plants.
Most soils have at least some residual nutrients. Only a soil test can assess this. Fertilizing without the results of a soil test leads to a waste of money and product, and can exacerbate an existing nutrient imbalance. In addition, sometimes nutrients are present in sufficient supply but are unavailable because of too high or too low pH. A soil test can reveal this, and a soil lab professional or crop consultant can recommend practices to resolve such problems.
Soil and fertilizer management tips for home gardeners
Some gardeners do not say that they garden, but rather that they work the soil. This reveals an understanding that good soil conditions are essential to support productive plant growth. Here are a few gardening tips related to soil management:
To amend a heavy (clayey) soil, add OM, not sand. As OM decomposes to humus, it “glues” particles together into aggregates, and improves drainage.
To amend a light (sandy) soil, add OM, not clay. OM increases sand’s ability to hold water and nutrients.
Most ornamental landscape plants (woody trees and shrubs, and herbaceous perennials and annuals) are best fertilized in spring. Fertilizing late in the season can lead to a late-season flush of growth that does not adequately harden off before winter.
Most houseplants are best fertilized at the rate recommended on the product label in spring and summer, and at half that rate in fall and winter.
Fertilize vegetable gardens by banding (place fertilizer alongside the crop row, 2” away and 2” deep in the soil) and/or by incorporating fertilizer into the soil in spring. Side-dressing supplemental nitrogen fertilizer next to growing plants later in the season may be necessary. Manage the pH of garden soil to ensure good nutrient availability. Rotate vegetable crops with cover crops to maintain good levels of organic matter, which helps the soil retain nutrients for plant use.
When fertilizing a lawn, determine the level of growth desired. If a low-maintenance lawn is desirable, no fertilizer may be needed. Slow-release fertilizers are preferred over soluble fast-release formulations. Apply a maximum of 2 pounds nitrogen per 1000 square feet per year on established lawns in most cases, apply half at spring green-up and half in fall (before September 15). Avoid fertilizing in midsummer. Leave an unfertilized buffer strip of at least 25 feet adjacent to lakes, streams, rivers, bays, vernal pools and wetlands. Avoid using phosphorus fertilizer if a soil test reveals phosphorus is not necessary, as phosphorus can cause freshwater quality problems. Reduce the amount of fertilizer needed by 1/3 to 1/2 each year by mowing with a mulching mower. Avoid weed-and-feed products, which do not allow the option to adjust the fertilize rate.
Avoid compacting soils. Walk on paths, keep garden carts on paths, park in the driveway rather than on the lawn, and avoid walking on one path across a lawn when it is frozen. Never walk on saturated soil. Wait until the garden dries out in spring before planting.
Avoid bare soil in your vegetable garden. When a crop is harvested, replant the area with another crop or plant a cover crop. Bare ground is prone to erosion and surface compaction by raindrops.
To assess whether a soil is adequately drained for many landscape plants, dig a hole 6” wide and 12” deep. Fill it to the top with water and let the water drain. Refill the hole with water, and time how long it takes to drain completely. If it drains within 3 hours, the soil is likely sandy. If it drains in 4-6 hours, drainage is adequate for a wide variety of plants. If some water remains after 8 hours, the soil is likely high in clay content and the site may retain too much moisture for some plants to thrive.
Why is SAR Important?
SAR indicates the suitability of water for use in agricultural irrigation. High levels of sodium ions in water affect the permeability of soil and can lead to water infiltration issues . While the impact severity of high SAR water depends on many specific soil quality factors (such as soil type, texture, drainage capacity, etc), typically the higher the SAR, the less suitable the water is for irrigation.
If your water has a high SAR, that generally means sodium in your water will cause hardening and compaction of your soil. This will reduce infiltration rates of both water and air. Additionally, the increased salinity reduces the availability of water in storage which can be very important for a plant’s growth and resilience (especially if you’re one who forgets to water sometimes).
Aside from decreased water infiltration and availability, high SAR may also lead to temporary over-saturation of surface soil, high pH, soil erosion, inadequate nutrient availability, and increased risk of plant diseases.
Concerned about your soil’s health? Tap Score can help with that, too! Take a look at these laboratory soil tests.
Collecting Soil Samples for Salinity Testing
The goal of salinity testing is to determine the salt level of soil from which roots extract water. Therefore, soil samples should be collected from the 0 to 6 inch depth or from the rooting depth. Deeper samples may be collected if the goal is to identify the extent of salinity caused by irrigation within the soil profile. In many cases, comparing soil samples from the affected area to surrounding normal-looking areas is valuable in diagnosing the problem. Collect eight to 10 cores from around a uniform area, mix them in a clean plastic bucket and transfer a composite sample (approximately 1 pound) to a soil sample bag.
The two alkali cations Na(+) and K(+) have similar relative abundances in the earth crust but display very different distributions in the biosphere. In all living organisms, K(+) is the major inorganic cation in the cytoplasm, where its concentration (ca. 0.1 M) is usually several times higher than that of Na(+). Accumulation of Na(+) at high concentrations in the cytoplasm results in deleterious effects on cell metabolism, e.g., on photosynthetic activity in plants. Thus, Na(+) is compartmentalized outside the cytoplasm. In plants, it can be accumulated at high concentrations in vacuoles, where it is used as osmoticum. Na(+) is not an essential element in most plants, except in some halophytes. On the other hand, it can be a beneficial element, by replacing K(+) as vacuolar osmoticum for instance. In contrast, K(+) is an essential element. It is involved in electrical neutralization of inorganic and organic anions and macromolecules, pH homeostasis, control of membrane electrical potential, and the regulation of cell osmotic pressure. Through the latter function in plants, it plays a role in turgor-driven cell and organ movements. It is also involved in the activation of enzymes, protein synthesis, cell metabolism, and photosynthesis. Thus, plant growth requires large quantities of K(+) ions that are taken up by roots from the soil solution, and then distributed throughout the plant. The availability of K(+) ions in the soil solution, slowly released by soil particles and clays, is often limiting for optimal growth in most natural ecosystems. In contrast, due to natural salinity or irrigation with poor quality water, detrimental Na(+) concentrations, toxic for all crop species, are present in many soils, representing 6 % to 10 % of the earth's land area. Three families of ion channels (Shaker, TPK/KCO, and TPC) and 3 families of transporters (HAK, HKT, and CPA) have been identified so far as contributing to K(+) and Na(+) transport across the plasmalemma and internal membranes, with high or low ionic selectivity. In the model plant Arabidopsis thaliana, these families gather at least 70 members. Coordination of the activities of these systems, at the cell and whole plant levels, ensures plant K(+) nutrition, use of Na(+) as a beneficial element, and adaptation to saline conditions.
Keywords: Channel Enzyme Membrane transport Plant Potassium Sodium Transporter Turgor.