Sinergias y trade-offs del secuestro de carbono con otros servicios de los agroecosistemas: una síntesis de literatura global

Comunicación oral presentada en: XVI Congreso Nacional de la Asociación Española de Ecología Terrestre. La Ecología en una biosfera humanizada. Almería, España. 16-20 octubre (2023)Las prácticas de manejo agrícola que incrementan el secuestro de carbono (C) promueven otros servicios de los agroecosistemas, como el mantenimiento de la estructura y la fertilidad del suelo o de la biodiversidad edáfica. Sin embargo, pueden incrementar la emisión de gases de efecto invernadero (GEIs) y la pérdida de nutrientes. Con el objetivo de revisar si las prácticas de secuestro de C muestran sinergias con la estructura y la biota edáficas, pero generan trade-offs en términos de emisión de CO2 y N2O o pérdidas de N y P, realizamos una síntesis de literatura global. Realizamos búsquedas sistemáticas de literatura para detectar artículos que evaluaran experimentalmente el efecto de minimizar la perturbación del suelo, diversificar los agroecosistemas y/o incrementar los aportes de materia orgánica frente a la utilización de prácticas convencionales. Detectamos 771 publicaciones, de las cuales incluimos 234 que analizaban 572 efectos en 228 sitios de 38 países. Las prácticas de manejo sostenible incrementaron el C en el suelo sin comprometer el rendimiento de los cultivos. El secuestro de C tuvo efectos positivos sobre la biota del suelo, más evidentes en términos de biomasa que de biodiversidad, así como sobre la agregación, porosidad, retención de agua y reducción de la compactación. Los efectos negativos del secuestro de C fueron en términos de emisión de CO2 y pérdida potencial de N. Discutiremos cómo estos efectos variaron entre prácticas de manejo, en el tiempo y el espacio, y revisaremos los principales vacíos de conocimiento detectados en la literatura

Development and analysis of the Soil Water Infiltration Global database

In this paper, we present and analyze a novel global database of soil infiltration measurements, the Soil Water Infiltration Global (SWIG) database. In total, 5023 infiltration curves were collected across all continents in the SWIG database. These data were either provided and quality checked by the scientists who performed the experiments or they were digitized from published articles. Data from 54 different countries were included in the database with major contributions from Iran, China, and the USA. In addition to its extensive geographical coverage, the collected infiltration curves cover research from 1976 to late 2017. Basic information on measurement location and method, soil properties, and land use was gathered along with the infiltration data, making the database valuable for the development of pedotransfer functions (PTFs) for estimating soil hydraulic properties, for the evaluation of infiltration measurement methods, and for developing and validating infiltration models. Soil textural information (clay, silt, and sand content) is available for 3842 out of 5023 infiltration measurements ( ∼ 76%) covering nearly all soil USDA textural classes except for the sandy clay and silt classes. Information on land use is available for 76% of the experimental sites with agricultural land use as the dominant type ( ∼ 40%). We are convinced that the SWIG database will allow for a better parameterization of the infiltration process in land surface models and for testing infiltration models. All collected data and related soil characteristics are provided online in *.xlsx and *.csv formats for reference, and we add a disclaimer that the database is for public domain use only and can be copied freely by referencing it. Supplementary data are available at https://doi.org/10.1594/PANGAEA.885492 (Rahmati et al., 2018). Data quality assessment is strongly advised prior to any use of this database. Finally, we would like to encourage scientists to extend and update the SWIG database by uploading new data to it

Soil sealing indicator for agricultural soils in Venezuela

Soil sealing is a degradation problem that involves different factors, processes and mechanics. Different methods and methodologies to assess those factors and processes can reflect different results and levels of soil structure degradation within the same soil, under different climate and management conditions. Standardized methods were evaluated for assessing soil sealing in five Venezuelan soils, with different texture and organic carbon content. The objective is to select indicators for predicting soil sealing. The results showed that the amount of water stable aggregates (WSA), the medium weight diameter (MWD) of the aggregates, the particles with diameter < 0.25mm (P250), the absolute sealing index (ASI), the consistency index (C5-10) and the soil losses from simulation rainfall were able to evaluate the stability of the soil surface structure. However when all the methods were compared based on the classification criteria of each method, the MWD and C5-10 had a discrepant class of soil sealing degradation when compared with other methods. The WSA, P250, ASI methods and soil characteristics as SOM chemical fractions and particles between 2 and 100 μm diameters, had high correlations among each other but all had good relationship with soil losses under simulated rainfall. From this study it can be concluded that a simple laboratory method is enable to evaluate soil surface sealing susceptibility but the method needs to be validated under field conditions as well