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Em4885 irrigation management practices to protect ground water

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4 CHAPTER<br />

Contact the local WSU Cooperative Extension or SCS offices for advice and assistance.<br />

Local agronomic consultants, <strong>irrigation</strong> supply centers, and agricultural engineers will also<br />

know which systems are best adapted <strong>to</strong> specific situations.<br />

IP 2.01.09 - Use Aerial Pho<strong>to</strong>graphy <strong>to</strong> Identify Patterns that Indicate<br />

Problems with Irrigation/Drainage Management<br />

Objective<br />

Early identification of crop development problems, some of which may be due <strong>to</strong> poor<br />

<strong>irrigation</strong> and drainage <strong>management</strong>.<br />

Description<br />

Aerial pho<strong>to</strong>graphy can be an aid in identifying overall problems in agriculture.<br />

Soil streaks, weed infestations, areas of insect pressure or plant disease, and <strong>irrigation</strong><br />

and drainage problems may be readily indicated by aerial observation. Modern techniques<br />

involve the use of infrared film and computer enhancement <strong>to</strong> increase the usefulness of<br />

aerial pho<strong>to</strong>graphy. Information about available aerial pho<strong>to</strong>graphy services can be found<br />

in local phone books or by contacting WSU Cooperative Extension or the SCS.<br />

SECTION 2 - PRACTICES FOR SURFACE (FURROW/RILL,<br />

BORDER STRIP) IRRIGATION SYSTEMS<br />

Drought Advisory EM4828, Surface Irrigation Systems, published by WSU Cooperative<br />

Extension is a discussion of achieving good distribution uniformity and application efficiency<br />

with surface <strong>irrigation</strong> systems.<br />

There are two variables that control how much <strong>water</strong> infiltrates during an <strong>irrigation</strong> using a<br />

surface <strong>irrigation</strong> system, 1) the infiltration rate of the soil and 2) the opportunity time. The infiltration<br />

rate is how fast <strong>water</strong> will soak in<strong>to</strong> a soil. Infiltration rates usually change throughout a season<br />

due <strong>to</strong> <strong>irrigation</strong>s and cultivations and normally decrease continuously throughout an <strong>irrigation</strong><br />

(although most soils will reach what is known as a “basic intake rate” at some point in the <strong>irrigation</strong>).<br />

Opportunity time is the amount of time that <strong>water</strong> is on the surface of the soil at a particular<br />

point. If <strong>water</strong> is running in a furrow for 24 hours, then the <strong>to</strong>p of the furrow has had 24 hours of<br />

opportunity time. The bot<strong>to</strong>m of the furrow has had something less than 24 hours because it takes<br />

time for <strong>water</strong> <strong>to</strong> travel from the <strong>to</strong>p of the furrow <strong>to</strong> the bot<strong>to</strong>m.<br />

There are three aspects of overall distribution uniformity with furrow/rill <strong>irrigation</strong> systems:<br />

1) down-row uniformity, 2) cross-row uniformity, and 3) soils variability. They are depicted in<br />

Figures 4-10, 11, and 12.<br />

36

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