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BaseStation 3200 User Manual – 11.7.5.15 ... - Baseline Systems

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<strong>BaseStation</strong> <strong>3200</strong> Advanced Irrigation Controller <strong>Manual</strong><br />

To understand soil moisture based smart irrigation, you also need to understand the following industry standard<br />

terms for soil moisture content.<br />

Drier Wetter<br />

Saturation<br />

Field Capacity<br />

Maximum<br />

Allowed<br />

Depletion (MAD)<br />

Permanent Wilt<br />

Point<br />

Oven Dry<br />

The soil pores are filled with water and nearly all of the air in the soil has been<br />

displaced by water. Gravity exerts force on the water contained in saturated<br />

soils, moving it deeper into the ground (if possible). When this “gravitational<br />

water” moves down through the soil, it becomes unavailable to plants.<br />

The level of soil moisture left in the soil after drainage of the gravitational<br />

water. If you irrigate to a level above field capacity, it will result in runoff or<br />

drainage as gravitational water.<br />

When the soil moisture content reaches this level, irrigation needs to start. In<br />

most cases, the maximum allowed depletion level is well before the plants<br />

begin to show visible signs of stress. Irrigators typically start watering at or<br />

before MAD is reached because they do not want their landscapes to show signs<br />

of stress.<br />

The minimal point of soil moisture where the plants wilt and begin to die off.<br />

When soil is dried in an oven, nearly all water is removed. This moisture content<br />

is used to provide a reference for measuring saturation, field capacity, and<br />

MAD.<br />

One key point is that water applied above field capacity is generally wasted – it gravitationally moves down<br />

through the soil and becomes unavailable to plants. Excess water will also leech nutrients from the soil into deeper<br />

soil layers, reducing the efficiency of fertilizers and soil treatments.<br />

To understand field capacity, it is often useful to think of a sponge. If you dunk a sponge in a bucket of water and<br />

pull it out, water will gravimetrically drain from the sponge for a period of time. When the dripping stops, the<br />

sponge will still be very wet. This moisture level is roughly equivalent to field capacity in soils – water is no longer<br />

draining into lower soil layers and is held in the root zone of the plants.<br />

When your irrigation system maintains soil moisture content between field capacity and maximum allowed<br />

depletion, you will find that your plants are healthier and your water use actually decreases. Studies also show that<br />

appropriately varying the time between irrigation events in order to allow the soil to dry to the chosen depletion<br />

point promotes deeper root growth and subsequently more efficiency and drought tolerance from the plants.<br />

How to Use Soil Moisture Sensors Successfully<br />

The first key for success with soil moisture sensors is to consider the hydrozones that exist in your landscaping. A<br />

hydrozone is a grouping of plants that have similar water usage and delivery characteristics and can be watered<br />

the same. For example, each of the following landscaping areas is a separate hydrozone:<br />

• Grass in full sun with rotors<br />

• Grass in full sun with sprays<br />

• Drip zones in full sun<br />

• Grass in shade with rotors<br />

• Grass in shade with sprays<br />

• Drip zones in shade<br />

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