tters. Besides, drip tube
systems are not trouble free: having the beds covered with fragile
pipes makes hoeing dicey, while every emitter must be periodically
checked against blockage.

When using any type of drip system it is especially important to
relate the amount of water applied to the depth of the soil to the
crops, root development. There's no sense adding more water than the
earth can hold. Calculating the optimum amount of water to apply
from a drip system requires applying substantial, practical
intelligence to evaluating the following factors: soil water-holding
capacity and accessible depth; how deep the root systems have
developed; how broadly the water spreads out below each emitter
(dispersion); rate of loss due to transpiration. All but one of
these factors--dispersion--are adequately discussed elsewhere in
_Gardening Without Irrigation._

A drip emitter on sandy soil moistens the earth nearly straight down
with little lateral dispersion; 1 foot below the surface the wet
area might only be 1 foot in diameter. Conversely, when you drip
moisture into a clay soil, though the surface may seem dry, 18
inches away from the emitter and just 3 inches down the earth may
become saturated with water, while a few inches deeper, significant
dispersion may reach out nearly 24 inches. On sandy soil, emitters
on 12-inch centers are hardly close enough together, while on clay,
30-or even 36-inch centers are sufficient.

Another important bit of data to enter into your arithmetic: 1 cubic
foot of water equals about 5 gallons. A 12-inch-diameter circle
equals 0.75 square feet (A = Pi x Radius squared), so 1 cubic foot
of water (5 gallons) dispersed from a single emitter will add
roughly 16 inches of moisture to sandy soil, greatly overwatering a
medium that can hold only an inch or so of available water per foot.
On heavy clay, a single emitter may wet a 4-foot-diameter circle, on
loams, anywhere in between, 5 gallons will cover a 4-foot-diameter
circle about 1 inch deep. So on deep, clay soil, 10 or even 15
gallons per application may be in order. What is the texture of your
soil, its water-holding capacity, and the dispersion of a drip into
it? Probably, it is somewhere in between sand and clay.

I can't specify what is optimum in any particular situation. Each
gardener must consider his own unique factors and make his own
estimation. All I can do is stress again that the essence of
water-wise gardening is water