Carbon stocks and soil attributes in Caatinga areas issued for different uses
Carbon stock. Soil management. Revegetation. Degraded area.
The vegetation of the Brazilian semi-arid is predominantly constituted by Caatinga. In recent
years, changes in the use of land, through anthropic practices such as livestock, firewood
extraction and mineration, have contributed for the degradation process of these areas, strongly
affecting the soil's capacity of store carbon. The benefits of revegetation in degraded areas
involve the entirety of the ecosystem and contribute to environmental balance. Based on this
context, this research aimed to evaluate the quality and carbon input of soils in areas under
native Caatinga vegetation, pasture, and in the process of revegetation for five years with native
species and Atriplex nummularia. In all areas, soil samples were collected at the end of the dry
and rainy seasons. Ten mini trenches 50 cm deep were opened, and soil samples were collected
(0-5, 5-10, 10-30, 30- 50 cm), for the purpose of evaluate the physics, chemical and biological
attributes of the soil. The pH in water (1:2,5), electrical conductivity and soluble cations (Ca2+
,
Mg2+
, Na+
, K+) in the soil samples will be determined. Soil density, granulometry and total
porosity will also be determined to evaluate the physical attributes. The contents of total organic
carbon (wet oxidation), carbon stock, water-soluble carbon, and labile carbon will be
determined according to the depth of the soil in areas under different vegetation covers. To
evaluate the biological quality, the contents of total organic carbon (wet oxidation), carbon
stock, carbon management index, permanganate oxidizable carbon as a function of soil depth
in areas under different vegetation covers. For the biological analyzes, samples were collected
only in the 0-5 cm layer and determined the microbial biomass carbon, soil metabolic quotient
(qCO2), microbial (qMic) and mineralization (qMin), respirometry, and humic substances, the
AH: AF and HUM ratio being calculated. The results indicated that the soil has a sandy texture,
with higher density for degraded pasture and revegetation areas. There were salt concentrations
and cation accumulation in the revegetation due to the history of degradation of the regenerated
area. CBM and C-Mic and RB differed between seasons, where the dry season presented higher
contents, The TOC and POC contents were higher in the rainy season and the POC still varied
between the areas, Caatinga> Revegetation> Degraded pasture, respectively. In relation to the
humic substances, in the surface layer, HUM> AH> AF. They also differed between seasons,
presenting higher values in the humid season. As well as the TOC stock, the lowest OC values
in the degraded pasture area suggest that management is negatively impacting soil organic
matter and quality. In general, it is possible to observe improvements in the area under
revegetation, even with the adversities that occur in the experimental area and that the areas
may take decades to be regenerated.