María Eugenia Carrizo

Aggregation agents and structural stability in soils with different texture and organic carbon contents

The flat pampas in the state of Santa Fe in Argentina have soils with high silt content, variable carbon content, and diverse degrees of structural degradation. Aggregate stability has been used as an indicator of the structural condition of the soil. This study aimed to quantify the effect of the addition of crop residues and root activity on the agents of aggregation and mechanisms of aggregate breakdown in soils with different carbon contents and textures cultivated under no-till. An experimental trial was conducted on a loamy soil (Typic Hapludoll, Santa Isabel series) and a silty soil (Typic Argiudoll, Esperanza series) under controlled conditions for 112 days with the following treatments: (i) with and without wheat plant growth and (ii) with and without addition of wheat residues. Soil structural stability by a method allowing for differentiation of aggregate breakdown by slaking, mechanical effect and microcracking, total organic carbon content, particulate organic carbon, glomalin and carbohydrate fractions was assessed. In general, the addition of residues and the presence of plant with active roots increased the presence of all aggregation agents and decreased aggregate breakdown processes in both soils. Soluble carbohydrates and proteins related to glomalin were the most important aggregating agents and their function was to reduce the magnitude of breakdown mechanisms, slaking and microcracking, evidencing a greater impact on the silty soil.

The intramolecular autoglucosylation of monomeric glycogenin.

The ability of monomeric glycogenin to autoglucosylate by an intramolecular mechanism of reaction is described using non-glucosylated and partially glucosylated recombinant glycogenin. We determined that monomer glycogenin exists in solution at concentration below 0.60-0.85 microM. The specific autoglucosylation rate of non-glucosylated and glucosylated monomeric glycogenin represented 50 and 70% of the specific rate of the corresponding dimeric glycogenin species. The incorporation of a unique sugar unit into the tyrosine hydroxyl group of non-glucosylated glycogenin, analyzed by autoxylosylation, occurred at a lower rate than the incorporation into the glucose hydroxyl group of the glucosylated enzyme. The intramonomer autoglucosylation mechanism here described for the first time, confers to a just synthesized glycogenin molecule the capacity to produce maltosaccharide primer for glycogen synthase, without the need to reach the concentration required for association into the more efficient autoglucosylating dimer. The monomeric and dimeric interconversion determining the different autoglucosylation rate, might serve as a modulation mechanism for the de novo biosynthesis of glycogen at the initial glucose polymerization step.

Evidence for glycogenin autoglucosylation cessation by inaccessibility of the acquired maltosaccharide.

Glycogenin initiates the biosynthesis of proteoglycogen, the mammalian glycogenin-bound glycogen, by intramolecular autoglucosylation. The incubation of glycogenin with UDP-glucose results in formation of a tyrosine-bound maltosaccharide, reaching maximum polymerization degree of 13 glucose units at cessation of the reaction. No exhaustion of the substrate donor occurred at the autoglucosylation end and the full autoglucosylated enzyme continued catalytically active for transglucosylation of the alternative substrate dodecyl-maltose. Even the autoglucosylation cessation once glycogenin acquired a mature maltosaccharide moiety, proteoglycogen and glycogenin species ranging rM 47-200kDa, derived from proteoglycogen, showed to be autoglucosylable. The results describe for the first time the ability of polysaccharide-bound glycogenin for intramolecular autoglucosylation, providing evidence for cessation of the glucose polymerization initiated into the tyrosine residue, by inaccessibility of the acquired maltosaccharide moiety to further autoglucosylation.

Spatial variability of short-term effect of tillage on soil penetration resistance

ABSTRACT The effect of tillage on soil properties varies within field due to spatial variability of soils. Mapping changes of soil penetration resistance (PR) would be useful to understand and assess tillage practices to alleviate soil compaction. The objectives were to model the short-term effect of tillage on PR and its spatial structure, and to delineate homogeneous zones based on soil response in a Typic Argiudoll previously managed under no-till. A grid sampling for PR and soil water content (SWC) were performed before and after chiselling. Spatial analysis was performed on the effect of tillage on PR data by 10 cm layers and homogeneous zones were delineated by k-means cluster analysis. The effect of tillage was −0.33 MPa in 10–20 and 20–30 cm layer. No differences of PR were found at 0–10 cm. Short range (5–7 m) spatial structure on the horizontal plane was observed in all layers. Only 45% of the field showed a marked effect of tillage on PR. Mapping the effect of tillage on PR would be a useful approach for evaluating the global and local response of soil to tillage, as well as for delineating of areas within field for site-specific tillage practices.