Fig.1-15 Effects of seawater salt (a) and solid coexistence (b) upon H2 generation (constant-height (1–cm) condition)
In seawater (a), Cl- and Br- ions affect H2 generation, making its amount larger than in pure water (PW). In submerged zeolites (b), pores and spaces affect H2 generation, leading to an enhancement that cannot be explained only by the water content within the zeolites.
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