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Soil CO2 efflux fluctuates in three different annual seasons in a semideciduous tropical forest in Yucatan, Mexico

El flujo de CO2 del suelo fluctúa en tres temporadas del año en un bosque tropical semideciduo de Yucatán, México

Fernando Arellano-Martín JUAN MANUEL DUPUY RADA ROBERTH ARMANDO US SANTAMARIA José Luis Andrade Torres (2022, [Artículo])

Tropical forest soils store a third of the global terrestrial carbon and control carbon dioxide (CO2) terrestrial effluxes to the atmosphere produced by root and microbial respiration. Soil CO2 efflux varies in time and space and is known to be strongly influenced by soil temperature and water content. However, little is known about the influence of seasonality on soil CO2 efflux, especially in tropical dry forests. This study evaluated soil CO2 efflux, soil temperature, and soil volumetric water content in a semideciduous tropical forest of the Yucatan Peninsula under two sites (flat areas close to and far from hills), and three seasons: dry, wet, and early dry (a transition between the rainy and dry seasons) throughout a year. Additionally, six 24-h periods of soil CO2 efflux were measured within these three seasons. The mean annual soil CO2 efflux was 4±2.2 μmol CO2 m-2 s-1, like the mean soil CO2 efflux during the early dry season. In all seasons, soil CO2 efflux increased linearly with soil moisture, which explained 45% of the spatial-temporal variation of soil CO2 efflux. Soil CO2 efflux was higher close to than far from hills in some months. The daily variation of soil CO2 efflux was less important than its spatial and seasonal variation likely due to small diel variations in temperature. Transition seasons are common in many tropical dry forests, and they should be taken into consideration to have a better understanding of the annual soil CO2 efflux, especially under future climate-change scenarios. © 2022 Mexican Society of Soil Science. All Rights Reserved.

EARLY DRY SEASON SOIL TEMPERATURE SOIL VOLUMETRIC WATER CONTENT TROPICAL DRY FOREST BIOLOGÍA Y QUÍMICA CIENCIAS DE LA VIDA BIOLOGÍA VEGETAL (BOTÁNICA) ECOLOGÍA VEGETAL ECOLOGÍA VEGETAL

Changes in soil organic carbon pools after 15 years of Conservation Agriculture in rice (Oryza sativa)-wheat (Triticum aestivum) cropping system of eastern Indo-Gangetic plains

C.M. Parihar Mahesh Gathala ML JAT (2023, [Artículo])

The present study was carried out at Dr. Rajendra Prasad Central Agricultural University, Samastipur, Bihar during 2021-2023 to focus on examining alterations in SOC pools resulting from conservation agriculture (CA) practices in R-W system in the eastern IGP, following the collection of soil samples from a long-term trial that was initiated in rainy (kharif) season 2006. The trial included eight combinations, namely: conventional tilled rice (Oryza sativa L.) and wheat (Triticum aestivum L.) (CTR-CTW); CT rice and zero till wheat (CTR-ZTW); direct seeded rice (DSR) and wheat on permanent raised beds (PBDSR-PBW); ZTDSR and CT Wheat (ZTDSR-CTW); ZTDSR and ZT wheat without residue (ZTDSR-ZTW-R); ZTDSR-ZT wheat with residue (ZTDSR-ZTW +R); unpuddled transplanted riceZTW (UpTR-ZTW) and ZTDSR-sesbania brown manure-ZTW (ZTDSR-S-ZTW). Results revealed that implementing zero tillage (ZT) combined with residue retention in rice and wheat cultivation led to enhanced levels of soil organic carbon (SOC) across all four fractions, namely very labile (CVL), labile (CL), less labile (CLL), and non-labile (CNL), in comparison to the continuous and rotational tillage practices. The tillage and residue management options significantly affected the lability index (LI) and C pool index (CPI), with zero-tillage and residue retention leading to lower LI and higher CPI values. The management practices significantly affected the C management index (CMI), with zero-tillage and residue retention showing the highest CMI values. Findings showed the potential of CA practices for enhancing soil C quality as well as C sequestration in soil of the Eastern IGP of India.

Carbon Management Index Soil Organic Carbon Fractions CIENCIAS AGROPECUARIAS Y BIOTECNOLOGÍA CONSERVATION AGRICULTURE SOIL ORGANIC CARBON ZERO TILLAGE

Historical use of water resources. Civil works evolution in Zacatecas state

Carlos Bautista-Capetillo Georgia González-Pérez Hiram Badillo-Almaraz (2021, [Artículo, Artículo])

Availability and demand are essential aspects for the human being when planning is made to provide water to the different sectors that may have need of it; still, the demand of suitable volume of water increases day by day, while the supply decreases gradually. In this inverse relationship, anthropogenic and environmental dynamics are decisive to guarantee the needs of the population, specifically due to the climatic transformations evidenced in recent decades. Throughout history, the state of Zacatecas has suffered the ravages of extreme environmental events, mainly those related to drought. Likewise, but on a lesser extent, severe floods have occurred that have caused socioeconomic damage. In this work, the climatic variations of temperature and precipitation and their influence on the evolution of hydraulic systems for the supply of drinking water in the municipality of Nochistlán de Mejía, Zacatecas are analyzed during the period 1930-2015.

drinking water supply historical development of waterworks climate and its transformations Abasto de agua potable desarrollo histórico de obras hidráulicas clima y sus transformaciones CIENCIAS FÍSICO MATEMÁTICAS Y CIENCIAS DE LA TIERRA CIENCIAS FÍSICO MATEMÁTICAS Y CIENCIAS DE LA TIERRA

Studies of plant hydraulics and water relations in mexican environments: adaptation, physiology, and applications

Estudios sobre hidráulica y relaciones hídricas de plantas en ambientes mexicanos: adaptaciones, fisiología y aplicaciones

RODRIGO MENDEZ ALONZO Mark Olson Horacio Paz Casandra Reyes García CELENE MARISOL ESPADAS MANRIQUE CLARA TINOCO OJANGUREN Santiago Trueba (2022, [Artículo])

Given the outstanding global progress of research on the hydraulic pathway in plants, and its important role as an indicator of plant mortality risk, we reviewed: (1) the adaptive basis of hydraulic traits and their importance for overall plant function; (2) the number of primary scientific articles on plant hydraulics that have been produced in Mexico in the last 40 years, (3) research related to specific environments in Mexico, and (4) the possible applications of plant hydraulics to natural resource management. Our systematic review included 83 articles. The number of publications per year steadily increased over time, reaching its maximum in 2021. Veracruz and Yucatán are the states where the majority of scientific articles on plant hydraulics have been produced, but for most states less than two publications on this subject appeared in ca. 40 years, and none was found for Oaxaca and Chiapas, the most biodiverse states. In plant hydraulics, the most studied biome in Mexico was the tropical dry forest, followed by crops; trees were the most studied growth-form, followed by herbaceous crops and epiphytes. We point to the need of enhancing research in the interface between plant hydraulic function and remote sensing, as well as developing applications in adaptive forest management and ecological restoration. We hope that this review may ignite a national collaborative effort to quantify critical traits that could inform the hydraulic functioning of Mexican ecosystems, particularly in the underrepresented and highly diverse states of Mexico. © 2022 Sociedad Botanica de Mexico, A.C. All rights reserved.

ADAPTATION DROUGHT VULNERABILITY ECOPHYSIOLOGY PLANT WATER RELATIONS SYSTEMATIC REVIEW BIOLOGÍA Y QUÍMICA CIENCIAS DE LA VIDA BIOLOGÍA VEGETAL (BOTÁNICA) ECOLOGÍA VEGETAL ECOLOGÍA VEGETAL

Soil moisture content and maize grain yield under conventional and conservation agriculture practices - results of short term field tests in liselo, Namibia

Christian Thierfelder (2023, [Artículo])

This article focuses on the results from trials developed to monitor the short-term effects of conventionally tilled systems versus CA on soil quality and crop productivity under conditions of the major cropping systems in central, north-central and north-eastern regions of Namibia. Conventional tillage (CT), Minimum tillage (MT), Minimum tillage, mulch (MT-M), Minimum tillage, rotation (MT-R) and Minimum tillage, mulch and rotation (MT-MR) were the primary treatments tested. Significant differences (p≤0.000) among the treatments were observed in the 0-60 cm soil profiles where MT-M plots had the highest soil moisture content (39.8 mm, Standard Error of Mean 0.2815) over the study period. A significant difference (p=0.0206) in grain yield was observed in the second season with CT plots yielding the highest grain yield (3852.3 kg ha-1, standard error of mean 240.35). Results suggest that CA has the potential to increase water conservation and contribute to reduction of the risk of crop failure. Climate change driven degradation under conventional tillage necessitate alternative sustainable tillage methods. Conservation tillage methods and conservation agricultural practices that minimize soil disturbance while maintaining soil cover need to be adopted more locally as viable alternatives to conventional tillage.

Grain Yield Soil Moisture Content CIENCIAS AGROPECUARIAS Y BIOTECNOLOGÍA CONSERVATION AGRICULTURE CONVENTIONAL TILLAGE GRAIN YIELDS SOIL WATER CONTENT MAIZE

Funcionalidad física de los arrecifes de coral en el Pacífico mexicano (Bahía de Los Ángeles, Bahía de La Paz, Bahía de Banderas y Bahías de Huatulco

Physical functionality of coral reefs in the mexican Pacific (Bahía de Los Ángeles, Bahía de La Paz, Bahía de Banderas y Bahías de Huatulco)

CLAUDIA REBECA NAVARRETE TORICES (2023, [Tesis de maestría])

Los corales son la base en la estructura y funcionamiento de los arrecifes. Sin embargo, en las últimas décadas, estos ecosistemas han sufrido un deterioro debido a presiones naturales, antrópicas y factores de gran escala como el cambio climático. En general, la cobertura de corales ha disminuido y aunque en algunos casos se ha observado su recuperación, la caracterización de la funcionalidad de la estructura física de los sistemas ha sido escasamente explorada. El presente trabajo evalúa la funcionalidad física de los arrecifes de coral en cuatro áreas a lo largo del Pacífico mexicano, empleando el Índice Funcional Arrecifal (IFA). El IFA considera la tasa de calcificación, la complejidad estructural y la abundancia de las especies de coral de en cada sitio; los valores que el índice puede adquirir varían de cero a uno, son valores cercanos a cero refieren a un arrecife con baja funcionalidad, mientras que los valores cercanos a uno indican un arrecife con alta funcionalidad. La cobertura coralina promedio de las cuatro áreas fue 35.62 ± 15.01%, siendo Bahías de Huatulco (BH) quien presentó la mayor cobertura coralina con 55.61 ± 21.94 %, mientras que Bahía de Los Ángeles (BLA) tuvo la menor cobertura coralina (17.16 ± 0.08 %). El IFA promedio de las áreas fue de 0.54 ± 0.12, y con base en el indicador, BH tuvo una mayor funcionalidad con un IFA de 0.68 ± 0.09, mientras que BLA tuvo una menor funcionalidad (0.34 ± 0.08). Los corales del género Pocillopora fueron los que mayor IFA aportaron en la mayoría de los sitios excepto en BLA que es representada por Porites panamensis. El coral con mayor coeficiente funcional (CF) fue Pocillopora grandis con 0.81, perteneciente a Bahía de Banderas (BB) y por ende fue el coral que mayor contribuyó al IFA en el área. El valor del IFA de 0.68 a lo largo del Pacífico mexicano, nos indica que tiene una alta complejidad estructural, debido a la forma de los corales Pocillopora que son clave para la permanencia de los arrecifes del área.

Corals are the basis for the structure and functioning of reefs. However, in recent decades, these ecosystems have suffered deterioration due to natural and anthropogenic pressures and large-scale factors such as climate change. In general, coral cover has decreased and although in some cases their recovery has been observed, the characterization of the functionality of the physical structure of the systems has been barely explored. This study evaluates the physical functionality of coral reefs in four areas along the Mexican Pacific, using the Reef Functional Index (IFA). The IFA considers the calcification rate, structural complexity, and abundance of coral species at each site; The values that the index can acquire vary from zero to one, values close to zero refer to a reef with low functionality, while values close to one indicate a reef with high functionality. The average coral cover of the four areas was 35.62 ± 15.01%, with Bahías de Huatulco (BH) having the highest coral cover with 55.61 ± 21.94%, while Bahía de Los Ángeles (BLA) had the lowest coral cover (17.16 ± 0.08%). The average IFA of the areas was 0.54 ± 0.12, and based on the indicator, BH had higher functionality with an IFA of 0.68 ± 0.09, while BLA had lower functionality (0.34 ± 0.08). Corals of the genus Pocillopora were the ones that contributed the highest IFA in most of the sites except in BLA, which is represented by Porites panamensis. The coral with the highest functional coefficient (CF) was Pocillopora grandis with 0.81, belonging to Bahía de Banderas (BB) and therefore was the coral that contributed the greatest to the IFA in the area. The IFA value of 0.68 along the Mexican Pacific indicates that it has a high structural complexity, due to the shape of the Pocillopora corals that are key to the permanence of the reefs in the area.

Corales, Pocillopora, Índice de función arrecifal, Pacífico mexicano Corals, Pocillopora, mexican Pacific, Reef Functional Index BIOLOGÍA Y QUÍMICA CIENCIAS DE LA VIDA OTRAS ESPECIALIDADES DE LA BIOLOGÍA OTRAS OTRAS

Modelado y acoplamiento de la conductividad eléctrica e hidráulica a partir de tomografía de rocas

Modeling and coupling of electrical and hydraulic conductivity from rock tomography

Miguel Ángel Martínez Rodríguez (2022, [Tesis de maestría])

En este trabajo se emplearon técnicas de modelado numérico para simular el flujo de corriente eléctrica y de fluido a través de medios porosos con el fin de determinar el factor de resistividad y la permeabilidad, así como la distribución de los campos de densidad de corriente eléctrica y velocidad de flujo. Para el modelado de flujo eléctrico se desarrolló un algoritmo basado en diferencias finitas, mientras que para el modelado hidráulico se empleó una librería reportada en la literatura, basada en el método de redes de Boltzmann. En ambos esquemas de modelado se establecieron condiciones en la frontera poro-grano para modelar los procesos físicos exclusivamente en el espacio poroso. Los valores estimados de factor de resistividad y de permeabilidad, así como la porosidad, se emplearon para estudiar las correlaciones entre estas propiedades a través de relaciones petrofísicas. Para esto, se propuso una expresión que relaciona la permeabilidad y la porosidad y, empleando una relación existente entre el factor de resistividad y la porosidad, se propuso también una relación directa entre la permeabilidad y el factor de resistividad. Las relaciones propuestas fueron aplicadas a los valores numéricos obtenidos para paquetes de esferas generados numéricamente y se encontró que se ajustan mejor a los datos en comparación con las relaciones más comúnmente utilizadas, especialmente para porosidades altas. Se mostró también que estas relaciones petrofísicas toman la forma de las relaciones más comunes conocidas cuando se trata con porosidades bajas. Valores obtenidos de imágenes digitales de un paquete de esferas sintético y una muestra de dolomita mostraron que las expresiones para porosidades bajas son suficientes para ajustar datos de medios porosos con porosidades menores a un valor entre 0.3 y 0.4. Finalmente, se analizaron el factor de resistividad, la permeabilidad, las relaciones petrofísicas, y las distribuciones espaciales y estadísticas de los campos vectoriales de flujo se analizaron para comparar los fenómenos de transporte eléctrico e hidráulico, encontrando que algunos factores, como la porosidad efectiva, son importantes en ambos fenómenos de flujo; mientras que otros, como la adherencia del fluido a las paredes del poro, son particularmente relevantes para el flujo hidráulico.

In this work, numerical modeling techniques were used to simulate the flow of electric current and fluid through porous media in order to determine the resistivity factor and permeability, as well as the distribution of electric current density and flow velocity fields. For electric flow modeling, an algorithm based on finite differences was developed, while for hydraulic modeling, a library reported in the literature, based on lattice Boltzmann method, was used. In both modeling schemes, pore-grain boundary conditions were established to model the physical processes exclusively in the pore space. The estimated values of resistivity factor and permeability, as well as porosity, were used to study the correlations between these properties through petrophysical relationships. An expression relating permeability and porosity was proposed and, using an existing relationship between the resistivity factor and the porosity, a direct relation between permeability and resistivity factor was also proposed. The proposed relations were applied to data obtained for numerically generated sphere packs and were found to fit the data better than the most commonly used relationships, especially for high porosities. It was also shown that these petrophysical relationships take the form of the most common relationships known when dealing with low porosities. Modeling data on digital images of a synthetic sphere pack and a dolomite sample showed that the expressions for low porosities are sufficient to fit data from porous media with porosities lower than 0.3 to 0.4. Finally, resistivity factors, permeabilities, petrophysical relationships, and spatial and statistical distributions of flow vector fields were analyzed to compare electrical and hydraulic transport phenomena, finding that some factors, such as the effective porosity, are important in both flow phenomena; whereas some other, such as the pore-wall adherence, are particularly relevant to hidraulic flux.

Física de rocas, modelado numérico, relaciones petrofísicas, fenómenos de transporte, factor de resistividad, permeabilidad, porosidad, tomografía de rocas, campos vectoriales, distribución estadística Rock physics, numerical modelling, petrophysical relations, transport phenomena, resistivity factor, permeability, porosity, rock tomography, vector fields, statistical distribution CIENCIAS FÍSICO MATEMÁTICAS Y CIENCIAS DE LA TIERRA CIENCIAS DE LA TIERRA Y DEL ESPACIO GEOFÍSICA GEOFÍSICA DE LA MASA SÓLIDA TERRESTRE GEOFÍSICA DE LA MASA SÓLIDA TERRESTRE