Paisajes geomorfológicos relacionados con la clasificación de los suelos en planicies y terrazas de Tabasco, México:

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BackgroundThe traditional ecological knowledge of land of the Ch’ol originary people from southeast Mexico forms part of their cultural identity; it is local and holistic and implies an integrated physical and spiritual worldview that contributes to improve their living conditions. We analyzed the nomenclature for soil classification used in the Mexican state of Tabasco by the Ch’ol farmers with the objective of contributing to the knowledge of the Maya soil classification.MethodsA map of the study area was generated from the digital database of parcels in the ejido Oxolotán in the municipality of Tacotalpa, to which a geopedological map was overlaid in order to obtain modeled topographic profiles (Zavala-Cruz et al., Ecosistemas y Recursos Agropecuarios 3:161–171, 2016). In each modeled profile, a soil profile was made and classified according to IUSS Working Group WRB (181, 2014) in order to generate a map of soil groups, which was used to survey the study area with the participation of 245 local Ch’ol farmers for establishing an ethnopedological soil classification (Ortiz et al.: 62, 1990). In addition, we organized a participatory workshop with 35 people to know details of the names of the soils and their indicators of fertility and workability, from which we selected 15 participants for field trips and description of soil profiles.ResultsThe color, texture, and stoniness are attributes important in the Ch’ol nomenclature, although the names do not completely reflect the visible characteristic of the soil surface. On the other hand, the mere presence of stones is sufficient to name a land class, while according to IUSS Working Group WRB (181, 2014), a certain amount and distribution of stones in the soil profiles is necessary to be taken into consideration in the name. Perception of soil quality by local farmers considers the compaction or hardness of the cultivable soil layer, because of which black or sandy soils are perceived as better for cultivation of banana, or as secondary vegetation in fallow. Red, yellow, or brown soils are seen as of less quality and are only used for establishing grasslands, while maize is cultivated in all soil classes.ConclusionsFarmers provided the Ch’ol nomenclature, perceived problems, and uses of each class of soil. Translation of Ch’ol soil names and comparison with descriptions of soil profiles revealed that the Ch’ol soil nomenclature takes into account the soil profile, given it is based on characteristics of both surface and subsurface horizons including color of soil matrix and mottles, stoniness, texture, and vegetation.

Objective: Apples cultivated in Mexico generally are smaller and softer than those produced in other geographical latitudes considered as optimal for apple production. The aim of this evaluation was determine the effect of applications with calcium, nitrogen, potassium, magnesium, sulfur and naphthaleneacetic acid (NAA), as well as the harvest date on the quality of apple fruits. Methodology ‘Golden Smoothie’ apple trees were treated foliarly with CaCl2 with and without NAA, and with a mixture of N, K, Mg and S or gypsum applied to soil for two years. Apples were harvested at 141 (regular harvest date), 161 (mid-late harvest) and 171 days (late harvest) after full bloom (DAFB) and evaluated for quality at harvest time and during their storage at 0°C for up to 179 days. Results: Foliar applications of CaCl2 significantly increased the calcium content in fruit and leaves, but fruit quality, including firmness, was not influenced. Fertilization of soil with the mixture of nutrients, including CaSO4, did not influence the fruit quality. Lately harvested fruit was 14.9% heavier but 17.1% softer than fruit picked at the commercial harvest date. Delaying of fruit harvest reduced about 43 d the storability of fruit. Based in these results, the relative softness of apples grown in Mexico is not related with its calcium content, hence unlikely to be overcome with the application of this mineral. Conclusions: Even in the control fruits, both seasons, the stored fruits do not show some physiological disorder as bitter pit

Nitrogen immobilization and remobilization from a fertilizer were determined by hydrolytic fractionation of organic nitrogen with 6 M HCI into acid-soluble distillable nitrogen (NSAD), acidsoluble nondistillable nitrogen (NSAnD) and nonhydrolysable nitrogen (NnH) on the Ap horizons of eight different soils from Myzeqe (Albania), eastern France, and tropical Mexico. The soils were fertilized with Ki5N03 and then incubated at 28°C and 80% of the water holding capacity for 1 month. Mineral N was removed by extraction with a solution of CaC12 after which rye grass was sown. The nitrogen taken up by rye grass was thus derived from soil organic matter. The three NSAD, NSAnD and NnH fractions participate in both immobilization and remobilization. The NSAnD fraction was shown to be the most active fraction. Remobilization of the biomass was greater in the sandy brown soils than in the clayey soils, in which intra-aggregate immobilization would predominate. Evidently, the physical and chemical properties of the soils have a real bearing on immobilization and remineralization of nitrogen fertilizer in cultivated soils.