Irrigation

In most years there are at least some periods of inadequate rainfall. Even a short dry spell can adversely affect crop yield and quality. Irrigation requirements differ somewhat among the various kinds of vegetable crops, but they all benefit from supplemental irrigation when needed. It is critical to manage soil moisture to provide an ample and steady supply of water to crops without overwatering. Table 13 lists periods of critical water need by vegetable crops. Special crop requirements will also be discussed in each crop section of this Guide. General irrigation guidelines are presented here.

Contact your local Extension office to determine what information is available in your state. There are also several knowledgeable irrigation equipment suppliers who serve the New England area who can be very helpful. As you begin to plan your irrigation program, keep in mind that it is usually best to look first at the highest value crops you grow as well as the anticipated increases in yield and income with the use of irrigation. When buying equipment and developing irrigation program, consider its effect on yield, expenses, and income, especially for your highest value crops.

General Irrigation Guidelines

Soil Moisture

Soil is saturated when all pore spaces are filled with water, such as after heavy rain or irrigation. When excess water drains from the pore space, soil reaches field capacity. At this point, water is held by the soil but remains available to plant roots. As water is lost through evapotranspiration, the remaining water is held more tightly by soil particles and becomes harder for plants to access. Eventually the water becomes so tightly bound to soil particles it is inaccessible to plant roots. This point is referred to as the permanent wilting point or wilting coefficient. Soil moisture in the range between field capacity and the wilting coefficient is usable by plants and is called available water, although moisture stress will occur as the lower end of this range is reached. It is advisable to begin irrigating vegetables before half the available water has been used. If soil moisture is depleted below this point, plants will be under increasing stress without visible wilt symptoms. Moisture stress can greatly reduce yield and cause numerous disorders such as tip burn of leafy crops and blossom-end rot in tomatoes and other fruits.

To achieve the most benefit from an irrigation system, it is necessary to apply the correct amount of water at the right time. This means replacing the water lost through ET and doing so before plants are under stress. The rate of ET is affected by a number of environmental factors including solar radiation, temperature, wind speed, and relative humidity. When it is hot, sunny, and windy with low relative humidity, up to 1/3" of water per day can be lost through ET. That is about 2" per week. When it is cool, cloudy, and damp with little wind, losses are low. As canopy area increases, evaporation from the soil decreases due to shading, but transpiration from the leaves increases and generally ET increases. If weeds are present, their leaf canopy increases ET losses to the detriment of the crop. Evaporation from the soil surface is reduced by the use of organic mulch and nearly eliminated under areas covered with plastic mulch.

Evaporation pans can be used to estimate ET loss. Pans should be filled with a measured amount of water, such as 1", and placed in or next to the field in a sunny spot. The loss of water from an evaporation pan will approximate the amount lost through ET. Although this is not exact, it provides a good indication of the rate of loss when sprinkler irrigation is used. When irrigation occurs, the evaporation pans should be filled with the same amount of water as was applied to the field.

It is important to know the amount of available water that a particular soil can hold. This varies considerably with soil type. For example, a slit or clay loam can hold several times as much available water as a sandy soil (Table 12). Soil organic matter can substantially increase a soil's ability to store available water. It has been estimated that for each percent of soil organic matter, water holding capacity may increase by about 1/2" per foot of soil depth. Soils with a high available water holding capacity need less frequent irrigation. However, when irrigated less frequently, a greater amount of water should be applied per application. 

Table 12: Available Water Holding Capacity Based on Soil Texture

When to Apply Water

In general, if you wait for crop symptoms (wilting) to decide when to irrigate, the crop will already be damaged. While experienced growers learn their soils and how they interact with water over seasons of experience, utilizing a soil moisture measuring device or sensor of some sort enables a grower to attach a number to their observations and track trends over time. Readings provided by sensors can also be utilized to fine tune irrigation management strategies and better manage the growing environment for specific plants.  Proper installations of sensors is critical for accurate readings. Sensors can quickly and easily be moved from one location to another in order to better understand the dynamics of soil moisture in relation to soil types, irrigation cycles, topographical changes, etc., so long as the installation instructions are followed along with each move.

Soil tensiometers for measuring soil moisture are available at a cost of $75-150. They can be purchased through several field equipment suppliers. To use a tensiometer, place the porous tube of the tensiometer at the depth you desire moisture measurement. You can calibrate your tensiometer to a particular soil so irrigation is done when the tension on the gauge reads a certain value (a number specific to your soil and the crop you are growing). A maximum value (usually 30-35) would be used for a sandy loam soil and this value may vary with the particular tensiometer purchased. In utilizing tensiometers, be certain you are aware of soil variability within a given field. Three to four tensiometers per field may be needed to adequately account for this variability and, in addition, two depths (commonly 6" and 12") may be necessary to adequately reflect the most critically stressed areas. The 6" unit indicates when soil moisture near the surface is being depleted (begin irrigating) and the 12" one shows when the moisture has moved to the bottom of the root zone (stop irrigating). In a drip irrigation system, a rule of thumb is to place the tensiometer about 6" from the tape at a depth of one-third the entire root zone. During irrigation, the tensiometer indicates when field capacity has been attained at the depth of the porous tube.

Another type of soil moisture sensor gaining popularity in the northeast is the granular matrix sensor. These sensors provides a reading based on the electrical resistance between two electrodes embedded in the granular matrix within the sensor. The more soil moisture available in the soil, the lower the resistance and the number on the reader, measured in kilopascals (kPa) or centibars. 

Established guidelines for maintaining soil moisture in specific crops and soil types are available. Using these recommendations, paired with visually observing the crop and soil, provides growers with additional information on which to base their irrigation decisions. In most soils, other than heavy clay, the decision to irrigate would generally happen in the range of 30-60 kPa. Differences in soil type should be considered when determining the appropriate range in which to irrigate.

This reinforces the importance of knowing your soil type, along with monitoring soil moisture and visually observing crops and soil to make an informed irrigation decision. Additionally, the irrigation method makes a difference as to when a grower might decide to irrigate. For example, overhead irrigation is recommended to begin when the available soil moisture is no less than 50%, whereas drip irrigation, taking comparatively longer to distribute substantial volumes of water, should be started before plant available water drops below 80%. 

When using drip irrigation on plastic-covered raised beds, during rain events where less than 1" of rain has fallen, run the drip irrigation system as normal.  When greater than 1" of rainfall has occurred, delay the application of water through the drip irrigation system.  

Critical Periods for Moisture Needs

Vegetable crops should not be under stress at any time. Each crop has its particular periods of critical moisture needs. In many crops (such as sweet corn, beans, and peas), the most critical period is during or just after flowering. These crops have flower development in a much more concentrated period of time. Other crops (tomato, peppers, eggplant, and potato) also have a critical moisture need during fruit or tuber development. Check individual crops for details (Table 13). Some crops, such as onions, potatoes, pumpkins, and winter squash, benefit from dry conditions at the end of the growing season when the crop is curing.

Table 13: Critical Periods of Water Need of Vegetable Crops

Water Application Rate

The application rate of irrigation should not exceed the infiltration and percolation rates of the soil. Infiltration is the entry of water through the soil surface and percolation is the downward movement of water through the soil. If the application rate exceeds either the infiltration or the percolation rate, water will accumulate on the surface and is subject to run-off and erosion. Soil compaction and crusting inhibits infiltration, percolation, and root growth. Building soil organic matter, reducing tillage, and controlling traffic reduces soil compaction and crusting. 

Frost Control

Early- or late-planted vegetables can be subjected to freezing temperatures in spring or fall. Using an overhead sprinkler system that applies about 1/10" of water per hour during periods when the air temperatures in the crop canopy are below freezing can reduce or prevent crop losses. Applying more or less water may be necessary depending on minimum temperature, length of freeze period, and wind speed. Be certain to start irrigating before the temperature reaches freezing and continue irrigating until ice melts. The degree of protection depends on wind speed and other factors. However, protection below 20°F has not been attained.