Physical properties of technosols as evapotranspiration covers on potash tailings piles.

The covering of potash tailings piles with technosols (artificial soils) is a modern and promising method for decreasing the saline drainage of these piles. In this context, it is important to determine whether technosols have appropriate physical properties for crop growth. In evapotranspiration covers, physical properties, such as bulk density, particle size distribution, total porosity, proportion of large pores, and available water are particularly important because they allow for robust crop growth, which subsequently determines the evapotranspiration capacity. However, few studies have been performed to assess the physical properties of technosols and their ability to act as evapotranspiration covers on potash tailings piles. Therefore, the present study aims to evaluate the physical properties of four different technosols made of municipal solid waste incineration bottom ash and coal combustion residues installed on a potash tailings pile located in Heringen, Germany. The total porosity, infiltration capacity, particle size distribution, bulk density, wettability, water retention curve, pH, electrical conductivity, and water content were determined. The pH of the technosols averaged 8.5, the electrical conductivity varied from 2.8 to 3.3 mS/cm, the mean bulk density was 1.21 g/cm³, the total porosity was 52.8%, and the rate of medium pores was 13.9% of the technosol volume. On average, the coarse fraction accounted for 42% of the technosol mass, whereas the fine fraction accounted for 52% of the sand-size particles, 43% of the silt-size particles and 5% of the clay-size particles. Likewise, no wetting restrictions for the technosols were found. To conclude, the different technosols present no limitations for crop growth, although the heavy metal contents of municipal solid waste incineration bottom ash and coal combustion residues should be considered in future studies.

Bridging Microbial Functional Traits With Localized Process Rates at Soil Interfaces.

In this review, we introduce microbially-mediated soil processes, players, their functional traits, and their links to processes at biogeochemical interfaces [e.g., rhizosphere, detritusphere, (bio)-pores, and aggregate surfaces]. A conceptual view emphasizes the central role of the rhizosphere in interactions with other biogeochemical interfaces, considering biotic and abiotic dynamic drivers. We discuss the applicability of three groups of traits based on microbial physiology, activity state, and genomic functional traits to reflect microbial growth in soil. The sensitivity and credibility of modern molecular approaches to estimate microbial-specific growth rates require further development. A link between functional traits determined by physiological (e.g., respiration, biomarkers) and genomic (e.g., genome size, number of ribosomal gene copies per genome, expression of catabolic versus biosynthetic genes) approaches is strongly affected by environmental conditions such as carbon, nutrient availability, and ecosystem type. Therefore, we address the role of soil physico-chemical conditions and trophic interactions as drivers of microbially-mediated soil processes at relevant scales for process localization. The strengths and weaknesses of current approaches (destructive, non-destructive, and predictive) for assessing process localization and the corresponding estimates of process rates are linked to the challenges for modeling microbially-mediated processes in heterogeneous soil microhabitats. Finally, we introduce a conceptual self-regulatory mechanism based on the flexible structure of active microbial communities. Microbial taxa best suited to each successional stage of substrate decomposition become dominant and alter the community structure. The rates of decomposition of organic compounds, therefore, are dependent on the functional traits of dominant taxa and microbial strategies, which are selected and driven by the local environment.

Methane Bubble Growth and Migration in Aquatic Sediments Observed by X-ray µCT.

Methane bubble formation and transport is an important component of biogeochemical carbon cycling in aquatic sediments. To improve understanding of how sediment mechanical properties influence bubble growth and transport in freshwater sediments, a 20-day laboratory incubation experiment using homogenized natural clay and sand was performed. Methane bubble development at high resolution was characterized by µCT. Initially, capillary invasion by microbubbles (<0.1 mm) dominated bubble formation, with continued gas production (4 days for clay; 8 days for sand), large bubbles formed by deforming the surrounding sediment, leading to enhanced of macropore connectivity in both sediments. Growth of large bubbles (>1 mm) was possible in low shear yield strength sediments (<100 Pa), where excess gas pressure was sufficient to displace the sediment. Lower within the sand, higher shear yield strength (>360 Pa) resulted in a predominance of microbubbles where the required capillary entry pressure was low. Enhanced bubble migration, triggered by a controlled reduction in hydrostatic head, was observed throughout the clay column, while in sand mobile bubbles were restricted to the upper 6 cm. The observed macropore network was the dominant path for bubble movement and release in both sediments.

Water balance assessment of different substrates on potash tailings piles using non-weighable lysimeters.

Water balance is an important tool to evaluate water deficit or excess in crop systems. However, few studies have evaluated the water balance of vegetation grown on the residues from potash mining because the high sodium chloride levels of the residues hinder agricultural development. Therefore, this study aims to measure the water balance components in eight non-weighing lysimeters installed on a potash tailings pile in Heringen (Werra), Germany. These lysimeters were filled with different mixtures of household waste incineration slags and coal combustion residues, resulting in 4 different substrates with two repetitions. Manual seeding was performed using 65% perennial ryegrass (Lolium perenne L.), 25% red fescue (Festuca rubra L.) and 10% Kentucky bluegrass (Poa pratensis L.). Environmental conditions were monitored using an automatic weather station; ground-level and 1-m-high rain gauges. Precipitation and drainage were recorded weekly following the initial saturation of the lysimeters. Water balance components were determined for two hydrological years based on the expression: ET (mm) = P - D, where ET = evapotranspiration, P = precipitation and D = drainage. In addition, evapotranspiration was studied using the standard FAO Penman-Monteith equation and Haude's method. The lysimeter water balance measured in 2014 revealed an actual evapotranspiration rate of 66.4% for substrate 1, 66.9% for substrate 2, 65.1% for substrate 3 and 64.1% for substrate 4. In 2015, evapotranspiration ranged from 65.7% for substrate 4 to 70.2% for substrate 1. We observed that the FAO Penman-Monteith and Haude's evapotranspiration models generally overestimated the water use of the green coverage by 67% and 23%, respectively. Our study suggests that an evapotranspiration cover for potash tailings piles may decrease brine drainage from these piles and reduce soil and water contamination.

Environmental factors affect the spatial arrangement of survival and damage of outplanted nothofagus dombeyi seedlings in the chilean andes / Factores ambientales afectan el arreglo espacial de la sobrevida y daño en plantas transplantadas de nothofagus dombeyi en los andes chilenos / Fatores ambientais afetam o arranjo espacial da sobrevida e dano em plantas transplantadas de nothofagus dombeyi nos andes chilenos

Mortality patterns were analyzed in a one-year old Nothofagus dombeyi plantation at mid-elevation in the Chilean Andes. Ripley´s univariate function was used to detect spatial patterns of mortality and damage (as reflected in crown dieback) of seedlings by assigning them into four categories: no crown damage, 1/3 of the crown damaged, 2/3 of the crown damaged and dead. Through correspondence analysis, variables (plant attributes, topography, weed competition, neighboring vegetation and fertilization) that could affect mortality were tested. At the end of the first growing season 67% of the seedlings survived, and by the end of the following dormant season only 37% were alive. Mortality patterns were random for seedlings with 1/3 of the crown damaged, and clustered for all other categories. Environmental variables with the greatest influence on mortality were increasing distance to a neighboring 10m tall plantation, absence of tall vegetation cover and convex micro-topography. Results suggest that large temperature oscillations with events of freezing temperatures (defined as the reported lethal temperature for 50% of its leaves) during the growing season, and severe frost during the dormant season, were the main causes of mortality and damage. The convenience of providing seedlings with some shelter when outplanted, or with an appropriate cold-acclimation treatment to resist low freezing temperatures when outplanted in open fields in harsh cold regions of the south-central Andes is discussed.

Se analizaron los patrones de mortandad en una plantación de Nothofagus dombeyi de un año de edad a altura media en los Andes chilenos. La función univariada de Ripley fue utilizada para detectar patrones espaciales de mortalidad y daño de las plantas asumiendo cuatro categorías: sin daño en la copa, 1/3 de copa dañada, 2/3 de copa dañada y muerte. Las variables (atributos de la planta, topografía, competencia de maleza, vegetación vecina y fertilización) fueron probadas por análisis de correspondencia. Al final de la primera estación de crecimiento 67% de las plantas sobrevivieron y al final del siguiente período latente solo 37% sobrevivían. Los patrones de mortalidad fueron aleatorios en plantas con 1/3 de la copa dañada, y agrupados en las otras tres categorías. Las variables ambientales con la mayor influencia en mortalidad fueron: distancia a una plantación vecina de 10m de altura, ausencia de cobertura vegetal alta y microtopografía convexa. Los resultados sugieren que grandes variaciones de temperatura con eventos de congelamiento (definido como la temperatura reportada como letal para 50% de las hojas) en la estación de crecimiento y congelamiento severo en la estación de latencia fueron las causas principales de mortalidad y daño. Se discute la conveniencia de proteger las plantaciones transplantadas o de una aclimatación apropiada para resistir las bajas temperaturas en plantas transplantadas a campo abierto en zonas frías de los Andes chilenos sur-centrales.

Analisaram-se os padrões de mortalidade em uma plantação de Nothofagus dombeyi de um ano de idade a altura média nos Andes chilenos. A função univariada de Ripley foi utilizada para detectar padrões espaciais de mortalidade e dano das plantas assumindo quatro categorias: sem dano na coroa, 1/3 de coroa danificada, 2/3 de coroa danificada e morte. As variáveis (atributos da planta, topografia, competência de maleza, vegetação vizinha e fertilização) foram provadas por análise de correspondência. No final da primeira estação de crescimento 67% das plantas sobreviveram e no final do seguinte período latente somente 37% sobreviviam. Os padrões de mortalidade foram aleatórios em plantas com 1/3 da coroa danificada, e agrupados nas outras três categorias. As variáveis ambientais com a maior influência em mortalidade foram: distância a uma plantação vizinha de 10m de altura, ausência de cobertura vegetal alta e microtopografía convexa. Os resultados sugerem que grandes variações de temperatura com momentos de congelamento (definido como a temperatura relatada como letal para 50% das folhas) na estação de crescimento e, congelamento severo na estação de latência, foram as causas principais de mortalidade e dano. Discute-se a conveniência de proteger as plantações transplantadas ou de uma aclimatação apropriada para resistir as baixas temperaturas em plantas transplantadas a campo aberto em zonas frias dos Andes chilenos sul-centrais.