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Soil organic carbon and nitrogen dynamics
under long-term conservation agriculture systems in Cambodia
Vira LENGa,b*, Rémi CARDINAELc, Vang SENGa, Florent TIVETa,c, d ,
Pascal LIENHARDc , d , Phearum Marka, Johan SIXe, Lyda HOKf, Stéphane Boulakiac,
Laurent THURIESg
a: Cambodian Conservat ion Agr i cul t ur e R esearch for Develop m ent C en ter , Department of Agr icu ltu ral Lan d
Res o urce s Man ag em ent, General Direct ora t e of Agriculture, Ministry of Ag ricult ur e , Forestry, and Fish eries,
Ph nom Pen h, C a mbodia
b: D o ctor al Sc hool GAIA, SupAgro Mon tpell i er, U ni versity of Montpelli er, Mo nt pe llier, France
c: AI DA , Univ Montpellier, CIRA D , M ont pellier, France
d: A g roec o logy and Safe Food System Tr an sitions in Southeast A sia Pro j ect (ASSET)
e: De partment of Environmenta l Systems Sciences, E TH Zur ich, 8092, Switzerland
f: Royal University of A gricu l tur e, Fa cult y of Agronomy and C enter of Excellence o n Su s taina ble Agricultural
Int ens ifi cat i on and Nutrition, Phnom P enh , Cambodia
g: CI RAD , U R Rec y cling and Risk, Avenue Agropolis, 34398, Mo ntp elli er , France
* C orrespo ndi n g a ut hor : leng vira@yahoo.com
This study quantified soil organic carbon (SOC) and soil total nitrogen (STN) changes in three long-
term (14 years) experiments comparing conventional tillage (CT) and different no-till (NT) cropping
systems using a diachronic approach and an equivalent soil mass approach. The three experiments
were established in 2009 in a randomized complete block design with three replicates and comprise
maize (MaiEx)-, soybean (SoyEx)-, and cassava (CasEx)-based cropping systems. Soil samples were
collected in 2021, 10 years after the first sampling (2011), at 7 depths: 0–5, 5–10, 10–20, 20–40, 40–
60, 60–80, and 80–100 cm. At 0–10 cm depth, NTs significantly increased SOC stock at a rate of
0.35, 0.51 and 0.73 Mg C ha-1 y-1 for CasEx, SoyEx and MaiEx, respectively. CT exhibited a positive
trend only on CasEx with an accumulation rate of 0.14 Mg C ha-1 y-1 (0-10 cm). A significant SOC
accumulation was observed under NT cropping systems for CasEX and MaiEx up to 60-80 and 80-
100 cm depth, respectively. By contrast, STN stock significantly increased under NT cropping
systems only at 0–5 cm depth with an accumulation rate of 13.9, 22.9 and 34.0 kg N ha-1 y-1 under
CasEx, SoyEx and MaiEx, respectively. A depletion of N stocks was observed under CT and NT
cropping systems at deeper soil layers. Over 10 years of time, SOC accumulation rate of NT, at 0-
100 cm depth, reached 1.08 and 1.73 Mg C ha-1 yr-1 for CasEx and MaiEx, respectively while non-
significant change was observed under NT SoyEx and CT of the three experiments. The findings
suggest that long-term NT cropping systems with high amount of biomass-C inputs and crop rotation
enhance SOC sequestration even at deeper soil layers. However, these results raise questions about
the dynamics of N under NT cropping systems.