“…Changes in the oxygen‐to‐carbon ratio of organic matter together with 13 C‐NMR data (Ward & Cory, ) give explicit evidence for the prominence of decarboxylation during photodegradation. This can occur when carboxylic acid groups are structurally close to the part of a molecule that absorbs radiation (e.g., Blake et al, ; Budac & Wan, ; Guzman et al, ; Schmitt‐Kopplin et al, ; Waggoner et al, ; Wang et al, ; Xu & Wan, ), with the aid of metal ions (e.g., Carraher et al, ; Faust & Zepp, ; Gao & Zepp, ; Gu et al, ; Miles & Brezonik, ), and in the presence of minerals (e.g., Miyoshi et al, ). These factors—structure of organic matter, metals, and minerals—likely determine the degree to which photodecarboxylation might occur in a soil.…”