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11,171 result(s) for "Anthropogenic soils."
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Anthropogenic soils are the golden spikes for the Anthropocene
We propose that the Anthropocene be defined as the last c. 2000 years of the late Holocene and characterized on the basis of anthropogenic soils. This contrasts with the original definition of the Anthropocene as the last c. 250 years (since the Industrial Revolution) and more recent proposals that the Anthropocene began some 5000 to 8000 years ago in the early to mid Holocene (the early-Anthropocene hypothesis). Anthropogenic soil horizons, of which several types are recognized, provide extensive terrestrial stratigraphic markers for defining the start of the Anthropocene. The pedosphere is regarded as the best indicator of the rise to dominance of human impacts on the total environment because it reflects strongly the growing impact of early civilisations over much of the Earth’s surface. Hence, the composition of anthropogenic soils is deemed more appropriate than atmospheric composition in providing ‘golden spikes’ for the Anthropocene.
Are anthropogenic soils from dumpsites suitable for arable fields? Evaluation of soil fertility and transfer of potentially toxic elements to plants
Background and purposeThe fertility of anthropogenic soils developed from dumpsites used for arable fields is not well-studied. The study aimed to evaluate the fertility of anthropogenic soils from an abandoned dumpsite in Awotan, Nigeria, by measurable indicators and the bioaccessibility of elements of selected plant species.MethodsThe study adopted multi-analytical approaches to determine the signatures of the soils and further parameterized the bioaccessibility of elements to plants.ResultsThe comparatively high content of Ca and Na in the anthropogenic soil contributed to the slightly alkaline soil reaction against the slightly acidic control. The high amount of organic matter is well-indicated by the enrichment of organic C and N in the anthropogenic soil. Waste deposition significantly contributed to the high accumulation of macronutrients (P, Ca, K, S) and micronutrients (Mn, Na, Fe) sufficient for maximum plant growth and yields, with an adequate C/N ratio supporting effective mineralization. The high cation exchange capacity of the anthropogenic soil contributed to cations binding. Indiscriminate waste deposition resulted in a high accumulation of potentially toxic elements (PTEs; Cu, Zn, As, Cd, Pb) above permissible limits in agricultural soils following WHO limits. Potential effects on lives are evident in the high PTEs accumulation in roots and leaves of Chromolaenaodorata, Saccopetalumtectonum, Passiflorafoetida, and Sennasiamea. These plant species exhibited various PTEs accumulation, especially for Cd and Pb.ConclusionAlthough anthropogenic soils remained fertile, the bioaccessibility of PTEs by plants indicates potential threats to consumers of crops and herbs produced from such sites.
Estimation of Organic Carbon in Anthropogenic Soil by VIS-NIR Spectroscopy: Effect of Variable Selection
Visible and near-infrared reflectance (VIS-NIR) spectroscopy is widely applied to estimate soil organic carbon (SOC). Intense and diverse human activities increase the heterogeneity in the relationships between SOC and VIS-NIR spectra in anthropogenic soil. This fact results in poor performance of SOC estimation models. To improve model accuracy and parsimony, we investigated the performance of two variable selection algorithms, namely competitive adaptive reweighted sampling (CARS) and random frog (RF), coupled with five spectral pretreatments. A total of 108 samples were collected from Jianghan Plain, China, with the SOC content and VIS-NIR spectra measured in the laboratory. Results showed that both CARS and RF coupled with partial least squares regression (PLSR) outperformed PLSR alone in terms of higher model accuracy and less spectral variables. It revealed that spectral variable selection could identify important spectral variables that account for the relationships between SOC and VIS-NIR spectra, thereby improving the accuracy and parsimony of PLSR models in anthropogenic soil. Our findings are of significant practical value to the SOC estimation in anthropogenic soil by VIS-NIR spectroscopy.
A review on anthropogenic soils from a worldwide perspective
Purpose This review focuses on what are referred to as “anthropogenic soils” (AS). It investigates and clarifies their descriptions, definitions, and classifications in terms of the following: (i) historical temporal trends in AS research worldwide, (ii) geographic distribution at various scales, (iii) dominant research themes, (iv) main site features, and (v) dominant anthropogenic processes. Materials and methods To assess the current status of AS research from an international perspective, an inventory of published studies on AS and related grey literature was prepared and compiled in an annotated bibliography, supported by an electronic database and coupled with a geographic information system. From an initial raw collection of over 3000 issues, 925 references published in the last 70 years (1945–2014) were considered a “representative population” of research focused on AS proper. Analysis of this source of information reveals that AS research is becoming increasingly consolidated. Indeed, it now represents an innovative field among soil sciences, expanding its conceptual scope and scientific production. Results and discussion AS research is spread over 64 different countries, mainly in Europe and North America. The USA is the most investigated country, with AS studies becoming extremely popular from 1965 to 1974 and increasing considerably thereafter. In all other countries, AS investigations only became very popular in the decade 1995–2004. On a worldwide scale, the most investigated urban areas (UA) are Berlin, Moscow, and New York City, while several important metropolises have been partially or entirely neglected. Interestingly, the review shows that although humans are able to significantly alter, transform, manipulate, and damage soil, with an incredible number of negative effects, the transformation of “natural” soils into AS may also have unexpected benefits. Conclusions It is hypothesized that AS research will become increasingly popular within the international scientific community over the next decades, with particular reference to those characterizing UA (such as Technosols). Finally, it is scientifically recognized worldwide how much AS can deviate from natural soils (in terms of physicochemical features, pedogenic processes, matter and energy fluxes). Therefore, we suggest definitively highlighting such differences, defining those parts of the pedosphere characterized by AS cover as the “anthropedosphere.”
Hydrochar from sugarcane industry by-products: assessment of its potential use as a soil conditioner by germination and growth of maize
BackgroundHydrothermal carbonization (HTC) is a thermochemical process to convert biomass in carbon-rich materials (hydrochar). The use of sugarcane industry by-products in HTC has been evaluated, generating a hydrochar rich in nutrients, which could be used as a soil conditioner. We raised the hypothesis that the application of hydrochar in soil can improve its nutrient characteristics, bringing a better environment and favouring plant growth, expecting a development similar to that one observed in anthropogenic soils.ResultsGermination studies were performed expecting a species-dependent response, using maize and tomato seeds, whose development was assessed in two soluble fractions obtained from hydrochar aiming to evaluate different rhizosphere conditions. The results showed a better development of maize, especially in the aqueous soluble fraction, whose nutrient concentration was lower than that of the acid soluble fraction, as well as the organic composition. Maize growth in soils showed a better initial development in ultisol compared to oxisol, this being inferred by root:shoot biomass ratio and by scanning electron microscopy (SEM) images. However, the development of maize was better in anthropogenic soil compared to soils that received hydrochar.ConclusionThe maize growth, compared with that carried out in anthropogenic soil, suggests that during the period evaluated the addition of hydrochar in soil did not have a negative effect upon maize development in its initial phase, and could have even favoured rooting in ultisol.
Anthropogenic Soils on the Territory of the New Jerusalem Monastery, Moscow Region
The soil cover inside the walls of the New Jerusalem Monastery (in the city of Istra, Moscow region) has been completely transformed during the long history of anthropogenic loads on the local landscape. Specific anthropogenic soils have been formed from the technogenic deposits on the top and slopes of the monastery hill. These soils contain numerous artifacts; in their upper part, horizons with characteristic features of the modern humus-accumulative process have been developed. The major types of anthropogenic soils on the territory of the monastery—urbiagrostratozems, soddy urbistratozems, and soddy-calcareous urbistratified soils—have been described. The composition of technogenic deposits determines the shift of pH values towards the alkaline reaction, the high content of available phosphorus compounds, and the soil contamination with heavy metals. The post-alluvial gray-humus soils close in their morphology and chemical properties to the natural soils of the floodplain predominate in the soil cover of the park zone adjacent to the walls of the monastery in the Istra River valley.
Proposal for a Quick Method for Choosing Plant Species to Accelerate Pedogenesis on Waste Dumps
Mining is one of the activities that require large areas of land for the storage of sterile rocks resulting from the extraction of useful mineral substances. Waste dumps are wide-spread, are unpleasant components of the landscape causing a negative visual impact, the modification of ecosystems and their functions, environmental pollution (depending on their content, it can result atmospheric pollution by entrainment of dust particles and powders by winds, generation of acid waters, land and soil pollution with trace elements, etc.), and may present risks for the objectives in the area as a result of the sliding potential. The waste dumps consisting of inert rocks like sands, clays, and dust in different mixtures, which present various degrees of aeration and permeability and which lack the fertility given by organic matter, need proper interventions and works to support the development of more valuable plants and to reintegrate them into the natural landscape. The research presented in this paper aims to identify the necessary steps in order to accelerate the pedogenesis process on mining dumps and, as a result, a logical scheme type method was developed that could be easily applied to any type of mining dump. Also, the logical scheme was applied and verified through an experimental study carried out at the level of the interior dump of North Pesteana open-pit from Rovinari mining basin, Romania.
Trait-based aerial dispersal of arbuscular mycorrhizal fungi
• Dispersal is a key process driving local-scale community assembly and global-scale biogeography of plant symbiotic arbuscular mycorrhizal (AM) fungal communities. A trait-based approach could improve predictions regarding how AM fungal aerial dispersal varies by species. • We conducted month-long collections of aerial AM fungi for 12 consecutive months in an urban mesic environment at heights of 20 m. We measured morphological functional traits of collected spores and assessed aerial AM fungal community structure both morphologically and with high-throughput sequencing. • Large numbers of AM fungal spores were present in the air over the course of 1 yr, and these spores exhibited traits that facilitate aerial dispersal. Measured aerial spores were smaller than average for Glomeromycotinan fungi. Trait-based predictions indicate that nearly one third of described species from diverse genera demonstrate the potential for aerial dispersal. Diversity of aerial AM fungi was relatively high (20 spore species and 17 virtual taxa), and both spore abundance and community structure shifted temporally. • The prevalence of aerial dispersal in AM fungi is perhaps greater than previously indicated, and a hypothesized model of AM fungal aerial dispersal mechanisms is presented. Anthropogenic soil impacts may liberate AM fungal propagules initiating the dispersal of ruderal species.
Urban areas, human health and technosols for the green deal
Authors aim to carry out a bibliographic review as an initial approach to state of the art related to the quality of urban soils, as well as its possible link with human health. This concern arises from the need to highlight the consequences that soil could face, derived from the growth and aging of the population, as well as its predicted preference for urban settlement. Urban development may pose a challenge to the health of urban soils, due to degradative processes that it entails, such as land take, sealing, contamination or compaction. A healthy soil is the one which maintains the capacity to support ecosystem services, so it can provide numerous benefits to human health and well-being (carbon sequestration, protection against flooding, retention and immobilization of pollutants and a growth media for vegetation and food production). This article addresses threats facing urban soils, the strategies put forward by the European Union to deal with them, as well as the issues that require further attention. Greening cities could be a consensual solution, so authors analyze whether soils of cities are ready for that challenge and what resources need to maintain soil ecosystem functions. This review proposes to use made by waste Technosols for a sustainable green city. Although the use of Technosols as a type of soil is very recent, the interest of the scientific community in this field continues to grow.