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PCC January/February 2018

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the crop for 10-14 days. Soil nitrate levels decline later in the<br />

crop cycle due to crop uptake and losses from leaching, and<br />

residual soil nitrate can be measured again prior to the next<br />

fertilization event to determine further fertilizer N needs. Residual<br />

soil nitrate levels of 20 ppm during the critical growth<br />

period following thinning indicates sufficient N is available<br />

for optimal crop growth. However, in the week prior to harvest<br />

soil nitrate levels can decline to below this level without<br />

jeopardizing crop yield.<br />

Nitrate in<br />

Irrigation Water<br />

Nitrate in irrigation water can also supply N for crop<br />

growth. The quantity of nitrate-N in irrigation water can be<br />

calculated from the following formula:<br />

ppm NO 3<br />

-N in irrigation water x 0.227 = lb N/acre inch of<br />

water<br />

Table 2 N in irrigation water and typical crop water usage<br />

ppm NO 3<br />

-N<br />

in irrigation<br />

lbs N/acre<br />

inch<br />

10 2.3 16 – 23<br />

20 4.5 32 – 45<br />

40 9.1 64 – 91<br />

60 13.6 95 – 136<br />

lbs N for a crop using<br />

7 – 10 acre inches water<br />

Nitrate in irrigation wells along the coast vary from less<br />

than 10 ppm NO 3<br />

-N to wells that have greater than 50 ppm<br />

NO 3<br />

-N. Calculating the quantity of N supplied by the irrigation<br />

water is made by multiplying the seasonal water uptake<br />

of the crop by the nitrate concentration of the water. Broccoli<br />

and cauliflower take up from 7-11 inches of water and lettuce<br />

5-9 inches of water. As can be seen in Table 2 waters supplying<br />

> 40 ppm NO 3<br />

-N can supply significant quantities of N<br />

for crop growth. In trials conducted in 2016-17, we observed<br />

that fertilization practices can be modified by a small amount<br />

(10 – 20 lbs N/A) with irrigation waters with < 20 ppm NO 3<br />

-N,<br />

however for wells with > 40 ppm NO 3<br />

-N, fertilization rates can<br />

be reduced more substantially (40 lbs to much more).<br />

Sources of Residual<br />

Soil Nitrate-N<br />

Levels of residual soil nitrate build up during production of<br />

the first crop which can result in substantial quantities of residual<br />

soil N at the beginning of the second crop. Residual soil<br />

nitrate-N comes from the following sources: mineralization of<br />

crop residues, unused fertilizer, NO 3<br />

-N in irrigation water and<br />

mineralization of soil organic matter. The quantity of N that<br />

remains in the field following harvest can be substantial (Table<br />

1, page 30) and can vary from 35 to >200 lbs N/A in spinach<br />

and broccoli, respectively. The concentration of N in crop residues<br />

varies from 2.5 to 5.0. Incubation studies of cool-season<br />

vegetable residues indicate more rapid mineralization of N with<br />

higher concentrations of N in the tissue; most mineralization<br />

Continued on Page 32<br />

<strong>January</strong>/<strong>February</strong> <strong>2018</strong><br />

www.progressivecrop.com<br />

31

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