Chemical oxygen demand fate from cottage cheese (acid) whey applied to a sodic soil

Abstract

Cottage cheese (acid) whey is an effective amendment in sodic soil reclamation, but the high chemical oxygen demand (COD) of whey is of concern in land application. The objective of this research was to determine the fate of COD from cottage cheese whey applied to a sodic soil. Treatments of 0, 25, 50, and 100 mm (0, 20, 40, and 80 Mg COD ha-1) of whey were applied to dry-unacclimated Freedom silt loam (fine-silty, mixed, mesic, Xerollic Calciorthids) in greenhouse lysimeters. The COD from lysimeter leachate at 1 m depth was monitored. Ninety days after whey application, total accumulative leachate COD for 0-, 25-, and 50-mm whey applications was not significantly different. Leachate COD concentrations from the 100-mm application reached 37% (29 400 mg COD L-1) of the applied whey COD. Twenty-eight days after whey treatment, infiltration was reduced in all whey-treated lysimeters, probably as a result of increased microbial activity. Barley (Hordeum vulgare L cv. Ludd) grain yield was 0.0, 0.0, 0.44, and 0.26 kg m-2 and total dry matter yield was 0.54, 0.72, 2.0, and 1.4 kg m-2 for the 0-, 25-, 50-, and 100-mm treatments, respectively. Salts and/or organic overloading appeared to inhibit initial barley growth in the 100-mm treatment. Results indicate a single 100-mm application to be excessive in terms of organic matter and/or salts

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