Dried and crushed 250gm soil samples (dried at 100 °C for 48 h) were passed through 2.0 mm sieve to remove roots and other aggregate matter. The soil chemical analysis was performed at the division of soil science, SKUAST-K Shalimar. pH was determined electrochemically with the help of glass electrode pH meter, as suggested by Jackson 1973. Exchangeable cations were extracted using 1 mol L−1 neutral ammonium acetate solution and quantified using the Kjeldahl method to measure the cation exchange capacity (CEC)37. The organic carbon of the soil samples was determined using the Walkley and Black method as outlined by38. Total nitrogen of the soils was determined using the Kjeldahl’s method following H2SO4 acid digestion method as suggested by38. The available K was determined from NH4OAc. (pH, 7.0) extract as described by38. The extract was analysed for available K by a flame analyzer at 589 nm. The available phosphorus was extracted from the soil with 0.5 M NaHCO3 (Olsen’s Method) at pH 8.5 and molybdo-phosphoric blue colour method of analysis was used for determination. Calcium and magnesium were estimated using atomic absorption spectrophotometer (AAS 4141) protocol using38. All quantified soil properties are given in Supplementary Table S1.
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