Determinants of the pHmito. Protons are pumped from the matrix to the IMS by the respiratory chain complexes I, III, and IV (green boxes) as electrons flow from reduced substrates in the matrix to O2. The pumping of electrically charged protons generates a ΔΨm of ∼180 mV and a pH gradient (ΔpHm: pHmito − pHIMS) of ∼0.9 pH units as the matrix becomes more alkaline than the IMS. The proton circuit is in thermodynamic equilibrium and changes in ΔΨm, thus causing opposing changes in ΔpHm by altering the energy required for the pumping of protons by respiratory chain complexes. ΔΨm and ΔpHm add up to generate a Δp used by the ATP synthase (blue-orange barrel) to generate ATP from ADP and Pi in the matrix. ΔΨm drives Ca2+ uptake across the mitochondrial Ca2+ uniporter (MCU; blue cylinder) and ADP–ATP exchange across the adenine nucleotide translocator (ANT; brown ovals). Electroneutral H+–ion exchangers rely exclusively on ΔpHm to extrude Ca2+, Na+, and K+ ions in exchange for protons (CHX, NHX, and KHX, respectively; brown ovals), whereas the PiC relies on ΔpHm to import the inorganic phosphate used for the synthesis of ATP (PiC; brown ovals). The coupling of H+ and ion fluxes implies that changes in the Na+, K+, Ca2+, and Pi gradients can alter ΔpHm. UCPs and the mPTP (UCPs and mPTP; blue cylinders) dissipate both ΔpHm and ΔΨm to generate heat and to initiate cell death, respectively. Variations in pHmito reflect the equilibrium between proton pumping by the respiratory chain; Δp dissipation by the ATP synthase, UCPs, and mPTP; ΔpHm dissipation by KHX, NHX, CHX, and PiC; and adaptive responses to changes in cytosolic pH and in ΔΨm.