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20 results for “humic”

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zenodo48/100

Humic acid like concentration in seawater samples, collected from the trace metal rosettes in the Southern Ocean during the austral summer of 2016/2017, on board the Antarctic Circumnavigation Expedition.

<p><strong>Dataset abstract</strong></p> <p>Humic acid like concentration (abbreviated HA) measured with respect to the Suwannee River Fulvic acid standards (&micro;mol SRFA equivalent per litre).</p> <p>Seawater samples were collected from trace metal rosette (TMR) deployments at different depths in the water column during the Antarctic Circumnavigation Expedition (ACE). Humic acid like data from legs 1 and 2, from TMR cast numbers 3 to 16, were analysed by electrochemistry following standard additions of Suwannee River Fulvic Acid (standard 1, IHSS). This data is to support iron ligands and iron bioavailability as well as hydrolysable saccharides (TPZT) data, also collected during ACE.</p> <p><strong>Dataset contents</strong></p> <ul> <li>ace_humics_data.csv, data file, comma-separated values</li> <li>ace_humics_data_visual_summary.png, metadata, portable network graphics</li> <li>data_file_header.txt, metadata, text format</li> <li>README.txt, metadata, text format</li> </ul> <p><strong>Dataset license</strong></p> <p>This humics dataset from ACE is made available under the Creative Commons Attribution 4.0 International License (CC BY 4.0) whose full text can be found at https://creativecommons.org/licenses/by/4.0/</p>

opencc-by-4.0Dec 2021View details →
edi48/100

Monthly monitoring of Fluorescence, UV, Humic and non-Humic Carbon, Carbohydrates, and DOC for Shark River Slough, Taylor Slough, and Florida Bay, Everglades National Park (FCE LTER) for January 2002 to August 2004

A better understanding of the biogeochemical cycling of nutrients in the Florida Coastal Everglades is a key issue regarding the restoration of the Everglades, which is expected to change the water quality throughout South Florida. In addition to rain, the main freshwater supply to Florida Bay will be derived from Taylor Slough and the C-111 Basin in the north-east section of the Bay. While it is known that these areas deliver significant amounts of nitrogen to the Bay, a significant portion of this nitrogen is in its dissolved organic form (DON). The sources, environmental fate and bioavailability to microorganisms of this DON are however, not known. Preliminary data suggest that although proteins have been detected in canal samples, labile dissolved organic matter (DOM) components were found to increase in abundance in the freshwater marshes compared to their levels in the adjacent canal waters. Leaching experiments of biomass showed the presence of such labile DOM. However, this DOM was found to be susceptible to both biodegradation and photodecomposition. In this study we will focus on the determination of the molecular characteristics of both DOM and DON and assess the bioavailability of these materials in transects ranging from the C-111 canal and Taylor Slough to the central part of Florida Bay. Relevant water quality and spectroscopic parameters will be monitored at 11 sites on a monthly basis, while six of these sites will be sampled biannually for DOM and DON chemical characterization and bioavailability studies. Advanced analytical techniques such as pyrolysis-GC/MS, FTIR, 13C- and 15N-NMR, gel electrophoresis and LC/MS will be used in the molecular characterization effort. We envisage that this study will allow for a better assessment of the sources of DON and its bioavailability in this system.

openCC (other)Jan 2006View details →
zenodo44/100

A dataset on ion-exchange membrane fouling by humic acid during electrodialysis

<p>This dataset decribes the effect of process setting on the fouling of an electrodialysis pilot installation treating a sodium chloride solution in the presence of humic acid in a series of 22 experiments. The electrical resistance over the electrodialysis stack was monitored in time while varying the crossflow velocity in the compartments, the current applied and the salt concentration in the processed. The active cycle was maintained for a maximum of 1.5h after which the polarity was reversed to remove the fouling layer. In the pilot, additional data is included such as the temperature, pH, flow rate, conductivity, pressure in the different compartments of the ED stack.</p>

opencc-by-4.0Nov 2019View details →
zenodo40/100

Text-fig. 3. Geological map and schematic geological section of the discovery site of the Late Upper Palaeolithic skull from Moča (southern Slovakia). I. – Primary position (?), II. – The discovery site (secondary position), A – B – The schematic geological section of the discovery site 1. H – Fluvial clayey to sandy loams (subordinately humolites) – Holocene; secondary discovery site layer, 2. lm-pH – Loam – peat – Holocene, 3. e Wl – Eolian sands – Late Würm (Late glacial of Würm), 4. lm,sWl – Fluvial clayey (to humic) loams or fine sands – Late Würm (Late glas cial of Würm); original discovery site layer, now eroded, 4a. fe Wl – Fluvial – aeolian silty sands (calcareous) – Late Würm (Late glacial s-lm of Würm), 5. lmW3 – Fluvial loams, sandy loams – final Würm (W3), 5a. W3 – Fluvial sands – final (?) Würm (?W3), 6. gW2+3 – Fluvial gravs els, sandy gravels, sands with gravel – Pleniglacial of Würm (W2+3), 7. lW – Aeolian loess and loess loams – Würm (undivided) in A Late Upper Palaeolithic Skull From Moča (The Slovak Republic) In The Context Of Central Europe

Text-fig. 3. Geological map and schematic geological section of the discovery site of the Late Upper Palaeolithic skull from Moča (southern Slovakia). I. – Primary position (?), II. – The discovery site (secondary position), A – B – The schematic geological section of the discovery site 1. H – Fluvial clayey to sandy loams (subordinately humolites) – Holocene; secondary discovery site layer, 2. lm-pH – Loam – peat – Holocene, 3. e Wl – Eolian sands – Late Würm (Late glacial of Würm), 4. lm,sWl – Fluvial clayey (to humic) loams or fine sands – Late Würm (Late glas cial of Würm); original discovery site layer, now eroded, 4a. fe Wl – Fluvial – aeolian silty sands (calcareous) – Late Würm (Late glacial s-lm of Würm), 5. lmW3 – Fluvial loams, sandy loams – final Würm (W3), 5a. W3 – Fluvial sands – final (?) Würm (?W3), 6. gW2+3 – Fluvial gravs els, sandy gravels, sands with gravel – Pleniglacial of Würm (W2+3), 7. lW – Aeolian loess and loess loams – Würm (undivided)

opencc-by-4.0Aug 2011View details →
dryad40/100

Dityrosine formation via reactive oxygen consumption yields increasingly recalcitrant humic-like fluorescent organic matter in the ocean

Open the record for dataset details and reuse information.

publicFeb 2020View details →
edi40/100

Response of humic acids and soil organic matter to vegetation replacement in subtropical high mountain forests

In this study, we used solid-state 13 C NMR spectroscopy, photometric analyses, and chemical fractionation to examine carbon (C) components and lability of SOM in a Japanese cedar (Cryptomeria japonica) forest and moso bamboo (Phyllostachys edulis) plantation reforested on a cutover primary broadleaf forest in Taiwan. The data was collected in Feb 2014.

openCC (other)Jul 2019View details →
zenodo36/100

Artificial humic acid diminishes the effect of drought on the soil microbiome

<p><span lang="EN-US">Humic substances have an enormous potential for regenerative agriculture to improve soil quality and plant growth. Recently developed technologies called hydrothermal humification enabled the conversion of waste into artificial humic acids, that would allow for sustainable and large-scale applications. However, not much is known about the effect of artificially produced humic acid on the soil microbiome, and its effect on drought-exposed soil. Therefore, we studied the effect of drought stress and artificial humic acid on the soil microbiota in sandy soil in a controlled experimental design. Analyses of 16S rDNA amplicon libraries by bioinformatics and statistics revealed that both, drought and artificial humic acid application, influenced bacterial community composition significantly, but only artificial humic acid affected bacterial diversity. Bacterial families like <em>Pseudomonadaceae</em>, <em>Peptostreptococcaceae</em> and <em>Moraxellaceae</em> enriched under artificial humic acid conditions, suggest an adaptation and selection of the soil bacterial microbiome. Under drought stress, artificial humic acid treatment kept bacterial diversity stable in the changed bacterial community composition. We propose that artificial humic acid application in sandy soil can improve the soil bacterial community, diminish drought stress, favor plant growth-promoting taxa, and bring enormous potential to sequestrate carbon in soil.</span></p>

opencc-by-4.0Dec 2024View details →
dryad36/100

Genomics of humic adaptation in Eurasian perch (Perca fluviatilis): SNP genotypes of 32 perch individuals, supplementary figures and tables

<p>Extreme <span>environments are inhospitable to the majority of species, but some organisms are able to survive in such hostile conditions due to evolutionary adaptations. For example, </span><span>m</span><span>odern bony fishes have colonized various aquatic environments, including perpetually dark,</span><span> hypoxic, hypersaline and toxic habitats</span><span>. </span><span>Eurasian perch (</span><em>Perca fluviatilis</em><span>) is among the few fish species of northern latitudes that is able to live in very acidic humic lakes. Such lakes represent almost "nocturnal" environments; they contain high levels of dissolved organic matter, which in addition to creating a challenging visual environment, also affects a large number of other habitat parameters and biotic interactions. To reveal the genomic targets of humic-associated selection, we performed whole-genome sequencing of perch originating from 16 humic and 16 clear-water lakes in northern Europe. We identified over 800,000 SNPs, of which &gt;10,000 were identified as potential candidates under selection (associated with &gt;3,000 genes) using multiple outlier approaches. Our findings suggest that adaptation to the humic environment may involve hundreds of regions scattered across the genome. Putative signals of adaptation were detected in genes and gene families with diverse functions, including organism development and ion transportation. The observed excess of variants under selection in regulatory regions highlights the importance of adaptive evolution via regulatory elements, rather than via protein sequence modification. Our study demonstrates the power of whole-genome analysis to illuminate multifaceted nature of humic adaptation and provides the foundation for further investigation of causal mutations underlying phenotypic traits of ecological and evolutionary importance.</span></p>

opencc-zeroMar 2022View details →
dryad36/100

Genomics of humic adaptation in Eurasian perch (Perca fluviatilis): SNP genotypes of 32 perch individuals, supplementary figures and tables

Open the record for dataset details and reuse information.

publicMar 2022View details →
zenodo32/100

datasets for "Atmospheric Humic-Like Substances (HULIS) Act As Ice-Nucleating Particles "

<p>These are datasets for manuscript titled &quot;Atmospheric Humic-Like Substances (HULIS) Act As Ice-Nucleating Particles&nbsp;&quot;</p>

opencc-by-4.0Dec 2020View details →
dryad32/100

Data from: A proteomic method to extract, concentrate, digest, and enrich peptides from fossils with colored (humic) substances for mass spectrometry analyses

Humic substances are break-down products of decaying organic matter that co-extract with proteins from fossils. These substances are difficult to separate from proteins in solution, and interfere with analyses of fossil proteomes. We introduce a method combining multiple recent advances in extraction protocols to both concentrate proteins from fossil specimens with high humic content, and remove humics, producing clean samples easily analyzed by mass spectrometry (MS). This method includes: 1) a non-demineralizing extraction buffer that eliminates protein loss during the demineralization step in routine methods; 2) filter-aided sample preparation (FASP) of peptides, which concentrates and digests extracts in one filter, allowing the separation of large humics after digestion; 3) centrifugal stage-tipping, which further clarifies and concentrates samples in a uniform process performed simultaneously on multiple samples. We apply this method to a moa fossil (~800¬–1000 yr) dark with humic content, generating colorless samples and enabling the detection of more proteins with greater sequence coverage than previous MS analyses on this same specimen. This workflow allows analyses of low-abundance proteins in fossils containing humics, and thus may widen the range of extinct organisms and regions of their proteomes we can explore with MS.

opencc-zeroJul 2019View details →
dryad32/100

Data from: A proteomic method to extract, concentrate, digest, and enrich peptides from fossils with colored (humic) substances for mass spectrometry analyses

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publicJul 2019View details →
zenodo28/100

OPTICAL DENSITY OF HUMIC ACIDS OF IRRIGATED SOILS OF BUKHARA OASIS

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opencc-by-4.0Dec 2023View details →
geo24/100

umami experiment-Analysis of the effect of amino-acids and humic substances on the transcriptome of Arabidopsis

GEO Series GSE297649. Arabidopsis thaliana. 9 samples. Type: Expression profiling by high throughput sequencing.

openGEO-OpenOct 2025View details →
zenodo24/100

Data for: On the adsorption mechanism of humic substances on kaolinite and their microscopic structure

<p>Soil organic matter (SOM) and various inorganic minerals represent key components of soils. During pedogenesis and due to biological activity these species interact, having a crucial impact on the formation of an aggregated soil structure with a hierarchical arrangement from nano to macro scale. In this process, the formation of organo&ndash;mineral microaggregates represents a dominant factor affecting soil functions and properties. This study focuses on the interactions between humic substances (HSs) and the mineral kaolinite as typical representatives of SOM and soil minerals. By performing classical molecular dynamics (MD) simulations on models of HSs and kaolinite, we demonstrate how two dominant but chemically different kaolinite surfaces affect the stability of HSs microaggregates. By analyzing volumetric, structural, and energetic properties of SOM&ndash;kaolinite models, we explain possible mechanisms of the formation of stable SOM&ndash;clay aggregates and show how a polarized environment affects the electrostatic interactions, stabilizing the microscopic structure of SOM&ndash;mineral aggregates. Our results showed that when stable aggregates of HSs are confined in kaolinite nanopores, their interactions with kaolinite surfaces disintegrate them into smaller subaggregates. These subaggregates are adsorbed more strongly on the polar aluminol surface of kaolinite compared to less the active hydrophobic siloxane surface.</p> <p>E. Galicia-Andr&eacute;s, C. Oostenbrink, M.H. Gerzabek and D. Tunega<br>On the adsorption mechanism of humic substances on kaolinite and their microscopic structure<br>Minerals 11 (2021), 1138<br>doi: <a href="https://doi.org/10.3390/min11101138">10.3390/min11101138</a></p>

opencc-by-4.0Oct 2021View details →
geo20/100

The complex interplay of genetic pathways in C.elegans following the treatment with humic substances

GEO Series GSE35360. Caenorhabditis elegans. 27 samples. Type: Expression profiling by array.

openGEO-OpenFeb 2012View details →
zenodo20/100

Raw_data_Morphological and physiological impact of humic substances on tomato growth under both non-stress and osmotic stress conditions

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openOct 2024View details →
zenodo20/100

Data for Ligand exchange provides new insight into the role of humic substances in the marine iron cycle

<p>This repository contains (i) all the data included in the study &quot;Ligand exchange provides new insight into the role of humic substances in the marine iron cycle&quot; in seven XSLX files, and (ii) twelve scripts and eight CSV files used to model the data with Dynafit software (http://www.biokin.com/dynafit/). A readme file is included to guide the calculations.</p> <p>The data sets originated when iron-saturated complexes of humic substances (fulvic acid and humic acid from the International Humic Substances Society) in seawater were subjected to iron ligand exchange after addition of an iron-free competing ligand, in most cases desferrioxamine B. In four cases EDTA and protoporphyrin IX were used as competing ligands to understand the effect of the chemical nature of the competing ligand. Additionally, reversibility was also tested. The concentration of the Fe-humic complexes was monitored by catalytic cathodic stripping voltammetry (10.4319/lo.2009.54.2.0610), a method not sensitive to the other iron species and free iron present.</p>

openzenodo-freetoread-1.0Jun 2023View details →
geo16/100

Transcriptional characterization of maize roots in response to nitrate (NO3-), Water-Extractable Humic Substances (WEHS) and NO3-+WEHS.

GEO Series GSE103184. Zea mays. 15 samples. Type: Expression profiling by array.

openGEO-OpenJul 2018View details →
geo16/100

The effect of phosphorus use efficiency affected by humic acid application on root gene expression in Rosa rugosa

GEO Series GSE311024. Rosa rugosa. 9 samples. Type: Expression profiling by high throughput sequencing.

openGEO-OpenNov 2025View details →

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