The study was conducted to study the effect of cattle grazing intensity on the deposition of organic carbon (Corg) in pasture soil. The work was carried out in 2010 on soddy-medium podzolic sandy loam soil in the Leningrad region. Three pasture areas were identified according to grazing intensity: weak (section 1), medium (section 2), strong (section 3). Corg and carbon in the clay fraction of the soil (Cclay) were determined according to the method of I. V. Tyurin. The sludge fraction (1 µm) was isolated using sedimentation and centrifugation. X-ray analysis of soil minerals was carried out in samples of the clay fraction of the soil on a DRON-3M diffractometer, Cu Kα tube mode 30 mA, 30 kV, from 3.5 to 75°, goniometer rotation speed 1° per minute. The soil of site 3 was distinguished by the minimum content of Corg in both periods of the survey (May – 16 C g/kg of soil; July – 27.8 C g/kg). The Corg value in the July samples was 1.3 times less compared to site 2 and 1.2 times less than site 1. Cclay values varied in the range: in May 40.8…108.9 C g/kg fractions, in July 99.7…140.9 C g/kg fraction. The content of Cclay in July samples from site 3 was 1.3 times higher than the content in samples from site 2 and 1.4 times from site 1. The variation in the enrichment coefficient (Esoc) was 1.78…3.50 in May, 2 in July .89…5.07. The highest Esoc was recorded for the soil of site 3 in July; its values exceeded the values in sites 1 and 2 by 1.75 times. The mineral depositing organic matter in the clay fraction of the soil of the site with high grazing intensity was mica with a deficiency of cations (r = 0.90). The increase in grazing intensity led to an increase in the content of Cclay.
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