Acidification and Nutrient Imbalances Drive Fusarium Wilt Severity in Banana (Musa spp.) Grown on Tropical Latosols
Fusarium wilt, caused by Fusarium oxysporum f. sp. cubense (FOC), remains a major
constraint to global banana (Musa spp.) production, especially in tropical regions. Although
soil conditions are known to modulate disease expression, the specific physicochemical
drivers of FOC prevalence under field conditions are not well understood. This study
investigated the relationships between soil properties and the Fusarium wilt incidence
across 47 banana farms on Hainan Island, China, a tropical region dominated by highly
weathered tropical soil (latosols). The disease incidence (%PDI) and FOC abundance
were quantified, alongside key soil parameters, including the pH, organic carbon, cation
exchange capacity, and macro- and micronutrient availability. The soils were predominantly
acidic (mean pH 4.93), with low levels of organic carbon and exchangeable calcium (Ca)
and elevated levels of available phosphorus (P), potassium (K), and magnesium (Mg). The
Fusarium wilt incidence ranged from 1% to 78%, with significantly higher levels observed in
younger plantations (<5 years old). Statistical analyses revealed strong negative correlations
between the PDI and the soil pH, exchangeable Ca and Mg, and available K. Principal
component analysis further confirmed the suppressive role of the pH and base cations in
the disease dynamics. Farms older than five years exhibited better soil fertility indices
and lower disease pressure, suggesting a temporal improvement in soil-mediated disease
suppression. These findings underscore the critical role of soil acidification and nutrient
imbalances, particularly Ca, Mg, and K deficiencies, in promoting FOC pathogenicity.
Enhancing soil health offers a promising and sustainable strategy for managing Fusarium
wilt in tropical banana production systems
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