Organic matter containing 0.2 millimoles of C is added to a 1 kg sample of deep water from the North Pacific. The bacteria in the sample respond and consume the organic matter, drawing down the dissolved oxygen as they respire (initial concentration of O₂ measured in the water before organic matter addition was 100 mol kg^-1). If we assume that the degradation of the organic matter follows Redfield stochiometric ratios: How much CO₂ will be produced (mol per kg)? How much dissolved inorganic nitrogen and dissolved inorganic phosphorous will be produced (in mol kg^-1)?