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Water‐stable aggregates and organic matter pools in a calcareous vineyard soil under four soil‐surface management systems
Author(s) -
Goulet E.,
Dousset S.,
Chaussod R.,
Bartoli F.,
Doledec A.F.,
Andreux F.
Publication year - 2004
Publication title -
soil use and management
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.709
H-Index - 81
eISSN - 1475-2743
pISSN - 0266-0032
DOI - 10.1111/j.1475-2743.2004.tb00376.x
Subject(s) - vineyard , calcareous , loam , soil water , soil organic matter , organic matter , total organic carbon , environmental science , agronomy , chemistry , soil structure , erosion , soil horizon , soil science , environmental chemistry , horticulture , botany , geology , biology , paleontology , organic chemistry
. Vineyards in Champagne, France are generally situated on slopes where the soils are subject to erosion. Therefore it is important to find a soil‐surface management practice that protects the soil against water erosion. We assessed the potential of mulches or grass covers to stabilize soil aggregates in a calcareous sandy loam from a vineyard in Champagne after 9 years under different management systems. Four different treatments were studied: (i) a bluegrass ( Poa pratensis ) surface cover between the vine rows (GC) with bare soil under the vines (R); two organic mulches of (ii) coniferous (CB) or (iii) poplar (PB) bark that covered the entire soil surface, and (iv) bare soil between the rows as a control. The bark amendments were applied every 3 years at rates of 61 and 67 t ha −1 for the PB and CB treatments, respectively. The kinetics of soil disaggregation in water fitted a power law ( A = K t − D ), in which K was the fraction of water‐stable >200 μm aggregates remaining after 1 hour of wet‐sieving. In the 0–5 cm layer, aggregate stability was greater for GC ( K =21.7), CB ( K =15.2) and PB ( K =13.6) than for the control ( K =10.5) and R ( K =11.8). In the 0–20 cm layer, CB also stabilized soil aggregates ( K =14.0–15.0); but PB did not. Structural stability was more strongly related to total organic carbon ( R 2 =0.64, P <0.001) than to microbial biomass carbon ( R 2 =0.54, P <0.001). A bluegrass cover enhanced structural stability in the 0–5 cm and 0–20 cm layers ( K =14.2), probably because of intense root development and rhizodeposition enhancing microbially produced metabolites, such as carbohydrates. Establishing grass cover or applying bark mulch are effective agricultural practices that improve soil aggregate stability and thus should reduce soil erosion. The vegetative growth of the vines was greater on the soils amended with bark mulches and less on the grass covered soils compared with the control soil; however, no difference in wine quality was observed among the different treatments.