“…These residues can result from agricultural practices in the field itself, as well as be derived from plants grown elsewhere. Starting with Jenny (1941), researchers have for decades gathered extensive data on the topic, not only in temperate climates but also in the tropics and arid regions (e.g., Bhattacharyya et al, 2021;Blet-Charaudeau et al, 1990;Gonzalez & Sauerbeck, 1982;Hans & Evans, 1957;Hénin et al, 1959;Hénin & Dupuis, 1945;Jenkinson, 1965Jenkinson, , 1971Jenkinson, , 1977Jenkinson, , 1990Jenkinson & Ayanaba, 1977;Jenkinson & Rayner, 1977;Ladd et al, 1985;Laudelout, 1993;Laudelout et al, 1960;Laudelout & Meyer, 1951;Mann, 1986;Poeplau et al, 2011;Smith et al, 1951;Smith et al, 2020;Soudi et al, 2020;Wiesmeier et al, 2020). The method of choice in much of this research has been to label organic matter isotopically with either 14 C or 13 C, then monitor the progressive decay of a single batch of that material over time after its incorporation into soils.…”