Feed the Future Innovation Lab for Collaborative Research on Aquaculture & Fisheries

The backbone of Java consists of chain at some 25 major volcanic peaks. Among the peaks are ridges of uplifted limestone reefs. Groundwater and runoff from volcanic regions were mineral poor carbonate-bicarbonate alkalinity was on the order of 20 mg L^-1. By contrast, waster emerging from limestone regions had alkalinity near 160 mg L^-1. When phosphorus and nitrogen fertilizers were added to low alkalinity water in ponds in a volcanic region, the growth of algae and subsequent yield of Nile Tilapia were low: 1.1 g C m^-1 day^-1 and 1080 kg fish ha^-1 per 150 day grow-out period respectively. With low alkalinity, carbon dioxide limited pond production, and phosphorus and nitrogen remained in pond water unused by the algae. When alkalinity was increased to 50-60 mg L^-1 and fertilizer was applied at the same rate, algae productivity and sh yield increased to 1.5 g C m^-2 day^-1 and 1475 kg fish ha^-1 per 150 day grow-out period. With increased abundance of CO2 and increased growth of algae, phosphorus and nitrogen uptake from pond water increased, thus improving fertilizer effciency. CO₂ continued to be in short supply at the highest levels of pond production obtained in the experiment. Fertilizer applied at the same rate to ponds in limestone drainage systems of Java with greater alkalinity would likely support pond productivity in excess of that obtained h ere. This work shows that CO₂ availability needs to be assessed during design of fertilizer application schemes in order to use fertilizers economically and to obtain consistent fertilizer-based yields from site to site in Java.

NOP 88-A02 (English)