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Aquifers

Aquifers are subsurface water-bearing geologic formations that can provide a reliable source of water for a variety of purposes, including drinking, irrigation, and industrial use.
These underground reservoirs are often found in porous and permeable rock or sediment layers, and their depth, size, and water quality can vary significantly depending on the local geology.
Researchers utilize advanced techniques, such as ai-driven comparisons, to study aquifer characteristics and identify the most effective protocols and products for aquifer research and management.
By enhancing reproducibility and accuracy, these tools can help simplify workflows and take aquifer studies to the next level.
Howver, understanding the complexities of aquifer systems remains an important challenge for scientists and water resource managers.

Most cited protocols related to «Aquifers»

Simulated genomes were generated from an initial set of 3604 draft genomes within IMG identified as being of high quality (see Supplemental Methods). To help alleviate bias toward well-sampled lineages, 280 of the 3604 high-quality draft genomes with identical phylogenetic marker genes were not used during the generation of simulated genomes. Simulated genomes were generated at varying degrees of completeness and contamination using three distinct random sampling models. Under the random fragment model, each contig comprising a genome was fragmented into nonoverlapping windows of a fixed size between 5 and 50 kbp. This size range was selected because it approximates the contig lengths of genomes recovered from metagenomic data or single-cell genomics: The mean N50 of the GEBA-MDM single-cell genomes, Wrighton acetate-amended aquifer population genomes, and Sharon infant gut population genomes is ∼28 kbp, ∼17 kbp, and ∼ 12 kbp, respectively. In order to generate genomes at a desired level of completeness and contamination, fragments were sampled without or with replacement, respectively. Windows were sampled until a simulated genome had completeness and contamination equal to or just greater than the target values. Generation of simulated genomes was limited to draft genomes as finished genomes were used to determine appropriate lineage-specific marker sets suitable for evaluating genomes (Fig. 3).
The 2430 draft reference genomes comprised of 20 or more contigs were used to simulate partial and contaminated genomes reflecting the characteristics of assembled contigs. Under this random contig model, genomes were generated by randomly removing contigs until the simulated genome reached or fell below a target completeness level. Contamination was introduced by randomly adding contigs with replacement from a single randomly selected genome until the desired level of contamination was reached or exceeded. These 2430 draft genomes were also used to generate genomes reflecting the limitations of metagenomic binning methods that rely on the statistical properties of contigs (e.g., tetranucleotide signature, coverage) to establish putative population genomes. To simulate this, partial genomes were generated by randomly removing contigs with a probability inversely proportional to their length until the simulated genome reached or fell below a target completeness level. Contamination was introduced by randomly selecting another draft reference genome and adding contigs from this genome with a probability inversely proportional to length until the desired level of contamination was reached or exceeded.
Publication 2015
Acetate Aquifers Genes Genome Infant Metagenome
An example of community-scale analyses including elemental biogeochemical cycling and sequential reaction analyses, functional network and metabolic Sankey visualization, and MW-score calculation were conducted using a metagenomic dataset of a microbial community inhabiting deep-sea hydrothermal vent environment of Guaymas Basin in the Pacific Ocean [53 (link)]. It contains 98 MAGs and 1 set of metagenomic reads (genomes were available at NCBI BioProject PRJNA522654 and metagenomic reads in NCBI SRA with accession as SRR3577362).
A metagenomic-based study of the microbial community from an aquifer adjacent to Colorado River, located near Rifle, has provided an accurate reconstruction of the metabolism and ecological roles of the microbial majority [2 (link)]. From underground water and sediments of the terrestrial subsurface at Rifle, 2545 reconstructed MAGs were obtained (genomes are under NCBI BioProject PRJNA288027). They were used as the in silico dataset to test METABOLIC’s performance. First, all the microbial genomes were dereplicated by dRep v2.0.5 [54 (link)] to pick the representative genomes for downstream analysis using the setting of “-comp 85.” Then, METABOLIC-G was applied to profile the functional traits of these representative genomes using default settings. Finally, the metabolic profile chart was depicted by assigning functional traits to GTDB taxonomy-clustered genome groups.
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Publication 2022
Aquifers COMP protocol Genome Genome, Microbial Hydrothermal Vents MAG protein, human Metabolic Profile Metabolism Metagenome Microbial Community Reconstructive Surgical Procedures Rivers

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Publication 2015
Aquifers arsenate Arsenic arsenite Dietary Fiber ferrihydrite Fluorescence Germanium goethite hematite illite mackinawite Magnetite orpiment Radiation Radiation Effects Radiography siderite
We used a ProEx (Dual Channel configuration) GPR produced by Malå Geosciences that was triggered by an electromechanic odometer and equipped with two shielded antenna pairs with central frequencies equal to 500 and 1600 MHz. In the present work, we will only show examples taken from the 500 MHz dataset. A Trimble GPS that recorded a fix every 10 seconds was used for the absolute data positioning. The mean trace interval equalled 15 cm.
In addition, a 51 mm diameter borehole that reached a depth of 5.68 m was drilled in the centre of the frost mound using a semi-portable core auger (Figs 1e and 2), exploiting the preliminary GPR results. The extracted core was stored at −20 °C at MZS prior to its delivery to the Beta Analytic laboratories (US) for 14C dating. During the coring, when we reached the first pocket of brine at 378 cm we interrupted the coring and collected brine in aquifer B1 using a peristaltic pump and sterile tubing. After collecting 5 litres of brine B1, we continued the core sampling of the following 12 cm and then re-inserted a new sterile tube to collect the brine from aquifer B2, which was located between 410 cm and 494 cm of depth. Finally, after collecting brine B2, we completed the core, reaching a depth of 568 cm.
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Publication 2016
Aquifers brine Figs Neoplasm Metastasis Obstetric Delivery Peristalsis Sterility, Reproductive

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Publication 2013
Alkalies Aquifers Biofilms Dietary Fiber Iron Manganese Metals Retention (Psychology) Rod Photoreceptors

Most recents protocols related to «Aquifers»

The study area of 1115.3
km2 is located in Northwestern Turkey within the Çanakkale
province (Figure 1).
Kirazlı village is located about 40 km southeast of the city
center and around the Biga Peninsula, which is an active tectonic
region. Mountainous topography features are seen in the region. Kirazlı
Mountain is the most important hill in the region, 811 m above the
sea level and covered with forests, which provides the main means
of livelihood for the local people. In this peninsula, alternating
reddish-yellow-white-colored volcanic and sedimentary rock formations
are commonly seen.41 (link) The former formations
are altered Neogene-age sedimentary covered with sand, silt, and clay,16 (link) and both formations are covered by quaternary
alluvium, including sand and gravel grains. In the rock structures
of the region, lead (Pb)–zinc (Zn)–copper (Cu) and gold
(Au) metal deposits and industrial minerals such as clay (Al2O3·2SiO2·2H2O), coal,
and kaolinite (Al2Si2O5(OH)4) have been identified.42 (link)In Çanakkale, Biga and some nearby towns
(Yenice, Can, and
Lapseki) are known for having a total of 204 metallic mineral deposits,
and the most important ones are Cu, Pb, Zn, antimony (Sb), and gold
(Au) reserves. Volcanic units at Kirazlı belong to the Miocene
age, which host alternating zones and precious metal mineralization
and contain feldspar, mafic minerals, and some quartz. The enrichment
of metals is Al + K in the argillic and Mg + Ca + Fe in the propylitic
alteration types. Moreover, two Au mineral deposit reserve places
are found—Kartal Dag and Maden Dag—and deposits of Fe
and Mn also have found been as small mass reserves. Environmental
changes (causing geogenic interaction between soil and water) affect
the enrichment and leaching of metals; for example, Ca, Mg, and Fe
were leached during argillic alteration, whereas strong Na leaching
is evident in all alteration types.43 (link)The hydrogeology of the Kirazlı region generally comprises
volcanic units. Most of the springs in the study area are between
the silicified zone and the argillic zone. Several springs surface
from volcanic soils such as tuff and agglomerate in the Biga Peninsula.
These springs have flow rates between 0.01 and 3 L/s. In the region
Çanakkale and Koca streams discharge into the Atikhisar Reservoir,
which serves the water supply system of Çanakkale city.41 (link) Generally, the main alluvial aquifers in the
region serve as the main water resources.41 (link) As seen in Figure 1, the study area has three types of geological structures. J1, J2,
and J3 represent, respectively, high mineral soil, low mineral soil,
and alluvial soil. While J1 includes evaporite mineral sedimentary
rocks such as gypsum and carbonates with high solubility only in acidic
waters, travertine, caliche, limestone, marble, and calcschist formations,
J2 consists of aluminum silicate-containing soils, conglomerates,
sandstone, and silica-predominant formations.44 X and Y in Figure 1 indicate the geologic coordinates, whereas W and S indicate water
and rock samples, respectively. The peninsula is in the Mediterranean
and Black Sea transition zone, affecting climate characteristics,
with summers being hot and dry and winters being cold and rainy. Maximum
precipitation is observed during the winter, whereas the least precipitation
is observed during summer.42 (link)
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Publication 2023
A 204 Aluminum Anabolism Antimony Aquifers Carbonates Cereals Clay Climate Coal Cold Temperature Copper feldspar Forests Gold Gypsum Kaolinite Limestone Marble Metals Minerals Natural Springs Patient Discharge Quartz Rain Silicates Silicon Dioxide Vision Water Resources Zinc
Uganda is a landlocked country lying within the equatorial region with a latitude of 1.3733° N, and a longitude of 32.2903° E. It occupies 241,550.7 Km2 of land, with open water and swamps constituting 41,743.2 Km2 [14 (link)]. Most of these water bodies are supplied by rainfall. Some rivers drain into wetlands while other wetlands arise from underground water trickling out of aquifers.
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Publication 2023
Aquifers Rivers Water, Body Wetlands
Sediment and fluid samples were collected in the summertime between 2019 and 2021 from geothermal springs and boreholes in the Biga Peninsula and in the vicinity of Edremit Town (Balikesir, Turkey) (Figure 1 and Supplementary Table 1). Hydrothermal sediments (Tuzla, Hidirlar, Büyükılıca, and Nebiler) were collected directly from the hot spring ponds using falcon tubes or with a shovel. Hot spring fluids (10–20 L) were collected from geothermal pools directly from the spring and immediately filtered (0.2 μm; Millipore Express, Merck, Darmstadt, Germany) from three sites, namely, Tuzla, Hidirlar, and Nebiler, using a peristaltic pump (Masterflex E/S 07571-05, Cole Parmer, USA). Several geothermal fluids were sampled from existing boreholes where deeply sourced hydrothermal aquifer water is constantly pumped to the surface. These fluids were collected either from a water collector (Güre 250 m-deep borehole) or directly from the pipe opening (Güre 1,390 m-deep borehole, Bardakcilar boreholes, Can, and Entur). Additional information on the fluid chemistry boreholes is found in Supplementary Table 1.
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Publication 2023
Aquifers Geothermal Springs Peristalsis

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Publication 2023
Aluminum Aquifers ARID1A protein, human Enzyme Multiplied Immunoassay Technique Freezing Light Minerals Odors Potassium Dichromate Rivers Sulfur
The area is located between the municipal solid waste incinerator belonging to the OLO company and the Slovnaft refinery in south-eastern part of Bratislava city, Slovakia. The incinerator was put into operation in 1978. There was no waste separation and recycling management in the past, and therefore, hazardous materials with high concentrations of trace metal (loid)s could be included in the incinerated waste. In the 80s, the MSWI ashes (both bottom and fly ashes) were loosely deposited close to the incinerator. The landfill area has never been properly closed and isolated from the surrounding environment. The MSWI ashes were partly covered by soil and vegetation grew over the landfill during the following years. The MSWI ashes have been exposed to the atmospheric conditions and plant exudates for over forty years. Moreover, illegal municipal and construction waste depositions were found in the area during its visual inspection. Most of the ash residues was recently removed and properly landfilled. A part of the MSWI ashes could not be removed as it is situated under the existing road. Besides that, several spots of the MSWI ashes, reaching a depth of ≥1 m, are still present in the study area. A new highway is currently crossing the old landfill and buildings are under construction in the area, with the surrounding being wooded. The area is a part of an environmental burden registered as “B2 (014)/Bratislava – Ružinov – incinerator – slag dump in front of the building (SK/EZ/B2/130)” in the Register of environmental burdens. The site is built by quaternary fluvial sediments consisting mostly of well-graded gravel, gravelly sands, fine sands and flood silt. The colour of gravel varies from brown to grey and the gravel diameter ranges from 1 cm to 10 cm. The gravelly sand layers consist mostly of gravel (60–77%) and sand (10–25%). The content of clay fraction is negligible. Fine sands of fluvial–aeolian origin are commonly deposited just below the soil layers. Their thickness reaches 4 m in some parts of the area. The total area covered by the ash was about 6100 m2. The groundwater table is detected at a depth of 1.8 m below the surface and is not in direct contact with MSWI ashes. The aquifer is in gravelly sands and characterised by an inter-granular permeability. The hydraulic conductivity and transmissivity coefficient of the aquifer are 6.13 × 10−3 m/s and 4.6 × 10−2 m2/s, respectively [35 ]. The direction of groundwater flow is from west to east and has been highly affected by the groundwater hydraulic protection system operated by the Slovnaft refinery since 1973 [36 ].
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Publication 2023
2'-deoxyuridylic acid Aquifers Ash Tree Clay Electric Conductivity Exanthema Exudate Floods Fly Ash Hazardous Substances Metals Permeability Plants Reproduction Transmission, Communicable Disease

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More about "Aquifers"

Aquifers are subsurface geological formations that serve as reliable underground reservoirs for water.
These porous and permeable rock or sediment layers can provide water for a variety of uses, including drinking, irrigation, and industrial applications.
Researchers utilize advanced techniques, such as AI-driven comparisons, to study aquifer characteristics and identify the most effective protocols and products for aquifer research and management.
By enhancing reproducibility and accuracy, these tools can help simplify workflows and take aquifer studies to the next level.
However, understanding the complexities of aquifer systems remains an important challenge for scientists and water resource managers.
Key subtopics in aquifer research include Sterivex filters, PowerWater DNA Isolation Kit, Supor filters, LM-485 7912 flow meters, Fluorescein dye tracers, PowerSoil DNA Isolation Kit, TD.06414 groundwater samplers, 5‐alpha‐cholestane internal standards, and Axioskop 2 plus microscopes with Mx3000P cyclers.
Advancements in AI-driven aquifer research, such as the use of PubCompare.ai, can help locate the best protocols from literature, pre-prints, and patents, ultimately enhancing the reproducibility and accuracy of aquifer studies.
By leveraging these powerful tools, researchers can simplify their workflows and take their aquifer investigations to new heights, tackling the complexities of these vital underground water resources.