cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.5281/zenodo.6320652
title: MOSSO_SoilChemistry_HistoricalSites_Annual_2008-2020

description: <strong>Abstract</strong> The dataset provides information about the soil chemical properties at two permanent LTER sites (named site 1 and 3, according to the LTER site numerations). The investigated period is 2008-2020. Details: Site 1 (coordinates: 45°52'22.43"N, 7°52'25.84"E; elevation: 2840 m a.s.l.) and Site 3 (coordinates: 45°52'13.52"N, 7°52'35.01"E; elevation: 2770 m a.s.l.). The bedrock is primarily micaschists, with some inclusions of amphibolites and calcschists. The vegetation of the sites is included in the ‘Siliceous alpine and boreal grasslands’ (habitat 6150, according to the EU Habitat Directive). At each site, consisting of paired plots for soil and vegetation survey, three 9 m<sup>2 </sup>plots are established, where three topsoil samples (A horizon, 0–10 cm depth) are collected annually at the end of the snow-free season (September). On soil samples the following analysis are performed: N-NH4, N-NO3, dissolved organic carbon (DOC), total dissolved nitrogen (TDN), dissolved organic nitrogen (DON), microbial carbon (Cmicr), and microbial nitrogen (Nmicr). <strong>Method Description</strong> Each soil sample consists of three subsamples that are homogenised by sieving at 2 mm. An aliquot of 20 g of fresh soil is extracted with 100 mL K2SO4 0.5 M, while 10 g are fumigated using chloroform for 18 h before extraction with 50 mL K2SO4 0.5 M. The concentration of DOC in not fumigated soil extracts (extractable DOC) is determined with a TOC analyzer (Elementar, Vario TOC, Hanau, Germany) after filtration with 0.45 μm nylon membrane filters. The microbial carbon (Cmicr) is estimated as the difference in extractable DOC between fumigated and non-fumigated samples, corrected using a recovery factor of 0.45 (Brookes et al. 1985, https://doi.org/10.1016/0038-0717(85)90144-0). Extractable N-NH4 concentration in soil extracts is measured spectrophotometrically (U-2000, Hitachi, Tokyo, Japan) using a modified Berthelot method based on the reaction with salicylate in the presence of alkaline sodium dichloroisocyanurate (Crooke and Simpson 1971, https://doi.org/10.1002/jsfa.2740220104). Extractable N-NO3 concentration in soil extracts is measured spectrophotometrically (U-2000, Hitachi, Tokyo, Japan) using the Greiss reaction (Mulvaney 1996, ISBN-10: ‎ 0891188258; ISBN-13: ‎ 978-0891188254) modified according to Cucu et al. (2014, https://doi.org/10.1007/s00374-013-0893-4). Extractable TDN is measured as reported for DOC. Extractable DON is determined as the difference between extractable TDN and inorganic nitrogen (extractable N-NH4 + N-NO3) in the extracts. Nmicr is estimated from the difference in extractable TDN between fumigated and non-fumigated samples corrected using a recovery factor of 0.54 (Brookes et al. 1985, https://doi.org/10.1016/0038-0717(85)90144-0). <strong>Instrumentation</strong> Spectrophotometer U-2000, Hitachi, Tokyo, Japan (N-NH4 and N-NO3) Elementar, Vario TOC, Hanau, Germany (DOC and TDN)
DOI: 10.5281/zenodo.6320677
title: MOSSO_SoilPhysics&Chemistry_AllSites

description: <strong>Abstract</strong> The dataset provides information about the soil physical and chemical properties at eight permanent LTER sites (named site 1, 2, 3, 6, 7, 8, 9, and 10, according to the LTER site numerations), located between 2686 (site 10) and 2854 m a.s.l. (site 6). Details: Site 1 (coordinates: 45°52'22.43"N, 7°52'25.84"E; elevation: 2840 m a.s.l.), Site 2 (coordinates: 45°52'22.17"N, 7°52'38.07"E; elevation: 2800 m a.s.l.), Site 3 (coordinates: 45°52'13.52"N, 7°52'35.01"E; elevation: 2770 m a.s.l.), Site 6 (coordinates: 45°52'32.21"N, 7°52'31.87"E; elevation: 2854 m a.s.l.), Site 7 (coordinates: 45°52'29.13"N, 7°52'44.71"E; elevation: 2813 m a.s.l.), Site 8 (coordinates: 45°52'27.74"N, 7°52'56.86"E; elevation: 2749 m a.s.l.), Site 9 (coordinates: 45°52'23.80"N, 7°53'3.96"E; elevation: 2720 m a.s.l.), and Site 10 (coordinates: 45°52'21.76"N, 7°53'9.32"E; elevation: 2686 m a.s.l.). The bedrock is primarily micaschists, with some inclusions of amphibolites and calcschists. The vegetation of the sites is included in the ‘Siliceous alpine and boreal grasslands’ (habitat 6150, according to the EU Habitat Directive). Each study site consists of paired plots for soil and vegetation survey. Soils belongs mainly to Regosol (sites 1 and 8), Leptosol (site 2), Cambisol (sites 6 and 7), and Umbrisol (sites 3, 9, and 10) great groups (IUSS Working Group WRB, 2015, E-ISBN 978-92-5- 108370-3.). On soil samples the following analyses are performed: pH, Cation Exchange Capacity (CEC), Total Organic Carbon (TOC), Total Nitrogen (TN), available phosphorous (Olsen P), and particle-size. <strong>Method Description</strong> The field description of the soil profile is done according to FAO (2006, ISBN 92-5-105521-1) while soil classification is done according to WRB classification system IUSS Working Group WRB, (2015 E-ISBN 978-92-5- 108370-3.). Soil material is collected from every horizon in the soil pit. The soil samples are air-dried, sieved to 2 mm, and analysed following the standard methods reported by Van Reeuwijk (2002, ISBN: 90-6672-044-1.). pH is measured in water (soil:water=1:2.5). Particle-size analysis is performed by the pipette method after organic matter destruction with H2O2 followed by dispersion with Na-hexametaphosphate. CEC is determined in a BaCl2 solution buffered at pH 8.1. TOC and TN are analysed by dry combustion with a CN elemental analyzer (CE Instruments NA2100, Rodano, Italy). Available P (Olsen P) is extracted with NaHCO3 and determined colorimetrically by the ascorbic acid molybdate blue method (Murphy and Riley 1962, https://doi.org/10.1016/S0003-2670(00)88444-5). <strong>Instrumentation</strong> WTW-InoLab 7110 pH-meter equipped with Hamilton GelGlass electrode (pH) CN elemental analyzer CE Instruments NA2100, Rodano, Italy (TOC and TN) Spectrophotometer U-2000, Hitachi, Tokyo, Japan (Olsen P)
DOI: 10.5281/zenodo.6320651
title: MOSSO_SoilChemistry_HistoricalSites_Annual_2008-2020

description: <strong>Abstract</strong> The dataset provides information about the soil chemical properties at two permanent LTER sites (named site 1 and 3, according to the LTER site numerations). The investigated period is 2008-2020. Details: Site 1 (coordinates: 45°52'22.43"N, 7°52'25.84"E; elevation: 2840 m a.s.l.) and Site 3 (coordinates: 45°52'13.52"N, 7°52'35.01"E; elevation: 2770 m a.s.l.). The bedrock is primarily micaschists, with some inclusions of amphibolites and calcschists. The vegetation of the sites is included in the ‘Siliceous alpine and boreal grasslands’ (habitat 6150, according to the EU Habitat Directive). At each site, consisting of paired plots for soil and vegetation survey, three 9 m<sup>2 </sup>plots are established, where three topsoil samples (A horizon, 0–10 cm depth) are collected annually at the end of the snow-free season (September). On soil samples the following analysis are performed: N-NH4, N-NO3, dissolved organic carbon (DOC), total dissolved nitrogen (TDN), dissolved organic nitrogen (DON), microbial carbon (Cmicr), and microbial nitrogen (Nmicr). <strong>Method Description</strong> Each soil sample consists of three subsamples that are homogenised by sieving at 2 mm. An aliquot of 20 g of fresh soil is extracted with 100 mL K2SO4 0.5 M, while 10 g are fumigated using chloroform for 18 h before extraction with 50 mL K2SO4 0.5 M. The concentration of DOC in not fumigated soil extracts (extractable DOC) is determined with a TOC analyzer (Elementar, Vario TOC, Hanau, Germany) after filtration with 0.45 μm nylon membrane filters. The microbial carbon (Cmicr) is estimated as the difference in extractable DOC between fumigated and non-fumigated samples, corrected using a recovery factor of 0.45 (Brookes et al. 1985, https://doi.org/10.1016/0038-0717(85)90144-0). Extractable N-NH4 concentration in soil extracts is measured spectrophotometrically (U-2000, Hitachi, Tokyo, Japan) using a modified Berthelot method based on the reaction with salicylate in the presence of alkaline sodium dichloroisocyanurate (Crooke and Simpson 1971, https://doi.org/10.1002/jsfa.2740220104). Extractable N-NO3 concentration in soil extracts is measured spectrophotometrically (U-2000, Hitachi, Tokyo, Japan) using the Greiss reaction (Mulvaney 1996, ISBN-10: ‎ 0891188258; ISBN-13: ‎ 978-0891188254) modified according to Cucu et al. (2014, https://doi.org/10.1007/s00374-013-0893-4). Extractable TDN is measured as reported for DOC. Extractable DON is determined as the difference between extractable TDN and inorganic nitrogen (extractable N-NH4 + N-NO3) in the extracts. Nmicr is estimated from the difference in extractable TDN between fumigated and non-fumigated samples corrected using a recovery factor of 0.54 (Brookes et al. 1985, https://doi.org/10.1016/0038-0717(85)90144-0). <strong>Instrumentation</strong> Spectrophotometer U-2000, Hitachi, Tokyo, Japan (N-NH4 and N-NO3) Elementar, Vario TOC, Hanau, Germany (DOC and TDN)
DOI: 10.5281/zenodo.6320676
title: MOSSO_SoilPhysics&Chemistry_AllSites

description: <strong>Abstract</strong> The dataset provides information about the soil physical and chemical properties at eight permanent LTER sites (named site 1, 2, 3, 6, 7, 8, 9, and 10, according to the LTER site numerations), located between 2686 (site 10) and 2854 m a.s.l. (site 6). Details: Site 1 (coordinates: 45°52'22.43"N, 7°52'25.84"E; elevation: 2840 m a.s.l.), Site 2 (coordinates: 45°52'22.17"N, 7°52'38.07"E; elevation: 2800 m a.s.l.), Site 3 (coordinates: 45°52'13.52"N, 7°52'35.01"E; elevation: 2770 m a.s.l.), Site 6 (coordinates: 45°52'32.21"N, 7°52'31.87"E; elevation: 2854 m a.s.l.), Site 7 (coordinates: 45°52'29.13"N, 7°52'44.71"E; elevation: 2813 m a.s.l.), Site 8 (coordinates: 45°52'27.74"N, 7°52'56.86"E; elevation: 2749 m a.s.l.), Site 9 (coordinates: 45°52'23.80"N, 7°53'3.96"E; elevation: 2720 m a.s.l.), and Site 10 (coordinates: 45°52'21.76"N, 7°53'9.32"E; elevation: 2686 m a.s.l.). The bedrock is primarily micaschists, with some inclusions of amphibolites and calcschists. The vegetation of the sites is included in the ‘Siliceous alpine and boreal grasslands’ (habitat 6150, according to the EU Habitat Directive). Each study site consists of paired plots for soil and vegetation survey. Soils belongs mainly to Regosol (sites 1 and 8), Leptosol (site 2), Cambisol (sites 6 and 7), and Umbrisol (sites 3, 9, and 10) great groups (IUSS Working Group WRB, 2015, E-ISBN 978-92-5- 108370-3.). On soil samples the following analyses are performed: pH, Cation Exchange Capacity (CEC), Total Organic Carbon (TOC), Total Nitrogen (TN), available phosphorous (Olsen P), and particle-size. <strong>Method Description</strong> The field description of the soil profile is done according to FAO (2006, ISBN 92-5-105521-1) while soil classification is done according to WRB classification system IUSS Working Group WRB, (2015 E-ISBN 978-92-5- 108370-3.). Soil material is collected from every horizon in the soil pit. The soil samples are air-dried, sieved to 2 mm, and analysed following the standard methods reported by Van Reeuwijk (2002, ISBN: 90-6672-044-1.). pH is measured in water (soil:water=1:2.5). Particle-size analysis is performed by the pipette method after organic matter destruction with H2O2 followed by dispersion with Na-hexametaphosphate. CEC is determined in a BaCl2 solution buffered at pH 8.1. TOC and TN are analysed by dry combustion with a CN elemental analyzer (CE Instruments NA2100, Rodano, Italy). Available P (Olsen P) is extracted with NaHCO3 and determined colorimetrically by the ascorbic acid molybdate blue method (Murphy and Riley 1962, https://doi.org/10.1016/S0003-2670(00)88444-5). <strong>Instrumentation</strong> WTW-InoLab 7110 pH-meter equipped with Hamilton GelGlass electrode (pH) CN elemental analyzer CE Instruments NA2100, Rodano, Italy (TOC and TN) Spectrophotometer U-2000, Hitachi, Tokyo, Japan (Olsen P)
DOI: 10.5281/zenodo.6320693
title: MOSSO_WaterChemistry_Lakes_Monthly_2007-2020

description: <strong>Abstract</strong> The dataset provides information about the monthly water chemistry of two high-elevation lakes: Bowditch Lake (coordinates: 45°52'30.52"N, 7°52'15.51"E, elevation: 2900 m a.s.l., lake area: 2400 m2) and Cimalegna Lake (coordinates: 45°52'23.17"N, 7°52'37.60"E, elevation: 2800 m a.s.l., lake area: 2700 m2). The Bowditch and Cimalegna lakes are located in the uppermost area and in the middle of the Cimalegna plateau, respectively. The bedrock of both lake catchments is mainly characterised by metamorphic rocks with a predominance of rocks with acid composition, and displaying the secondary presence of basic and terrigenous-carbonatic rocks. Soil (often vegetated) is the main land cover type in the Cimalegna Lake catchment, while coarse sediment constitutes the main land cover type in the Bowditch Lake catchment. Lakes are sampled from 3 points on the shore with no vegetation, at ca. 10-cm depth. The analysed water chemical parameters are: N-NH4 and N-NO3 (period 2007-2020); dissolved organic carbon (DOC), total dissolved nitrogen (TDN), and dissolved organic nitrogen (DON) (period 2011-2020); pH and electrical conductivity (EC) (period 2015-2020). <strong>Method Description</strong> The analyses are performed in the laboratory on filtered samples (0.45 μm, nylon). N-NH4 is determined spectrophotometrically (Spectrophotometer U-2000, Hitachi, Tokyo, Japan) by a modified Berthelot method involving reaction with salicylate in the presence of alkaline sodium dichloroisocyanurate (Crooke and Simpson 1971, https://doi.org/10.1002/jsfa.2740220104). N-NO3 is determined spectrophotometrically by the Greiss reaction as described by Mulvaney (1996, ISBN-10: ‎ 0891188258; ISBN-13: ‎ 978-0891188254) and modified by Cucu et al. (2014, https://doi.org/10.1007/s00374-013-0893-4). DOC and TDN are determined by a TOC analyzer (Elementar, Vario TOC, Hanau, Germany). DON is determined as the difference between TDN and inorganic nitrogen (N-NH4 + N-NO3). pH is measured potentiometrically using a WTW-InoLab 7110 pH-meter equipped with Hamilton GelGlass electrode. EC at 20°C is measured using a Crison - Micro CM 2201. <strong>Instrumentation</strong> Spectrophotometer U-2000, Hitachi, Tokyo, Japan (N-NH4 and N-NO3) Elementar, Vario TOC, Hanau, Germany (DOC and TDN) WTW-InoLab 7110 pH-meter equipped with Hamilton GelGlass electrode (pH) Crison - Micro CM 2201 (EC)
DOI: 10.5281/zenodo.6320692
title: MOSSO_WaterChemistry_Lakes_Monthly_2007-2020

description: <strong>Abstract</strong> The dataset provides information about the monthly water chemistry of two high-elevation lakes: Bowditch Lake (coordinates: 45°52'30.52"N, 7°52'15.51"E, elevation: 2900 m a.s.l., lake area: 2400 m2) and Cimalegna Lake (coordinates: 45°52'23.17"N, 7°52'37.60"E, elevation: 2800 m a.s.l., lake area: 2700 m2). The Bowditch and Cimalegna lakes are located in the uppermost area and in the middle of the Cimalegna plateau, respectively. The bedrock of both lake catchments is mainly characterised by metamorphic rocks with a predominance of rocks with acid composition, and displaying the secondary presence of basic and terrigenous-carbonatic rocks. Soil (often vegetated) is the main land cover type in the Cimalegna Lake catchment, while coarse sediment constitutes the main land cover type in the Bowditch Lake catchment. Lakes are sampled from 3 points on the shore with no vegetation, at ca. 10-cm depth. The analysed water chemical parameters are: N-NH4 and N-NO3 (period 2007-2020); dissolved organic carbon (DOC), total dissolved nitrogen (TDN), and dissolved organic nitrogen (DON) (period 2011-2020); pH and electrical conductivity (EC) (period 2015-2020). <strong>Method Description</strong> The analyses are performed in the laboratory on filtered samples (0.45 μm, nylon). N-NH4 is determined spectrophotometrically (Spectrophotometer U-2000, Hitachi, Tokyo, Japan) by a modified Berthelot method involving reaction with salicylate in the presence of alkaline sodium dichloroisocyanurate (Crooke and Simpson 1971, https://doi.org/10.1002/jsfa.2740220104). N-NO3 is determined spectrophotometrically by the Greiss reaction as described by Mulvaney (1996, ISBN-10: ‎ 0891188258; ISBN-13: ‎ 978-0891188254) and modified by Cucu et al. (2014, https://doi.org/10.1007/s00374-013-0893-4). DOC and TDN are determined by a TOC analyzer (Elementar, Vario TOC, Hanau, Germany). DON is determined as the difference between TDN and inorganic nitrogen (N-NH4 + N-NO3). pH is measured potentiometrically using a WTW-InoLab 7110 pH-meter equipped with Hamilton GelGlass electrode. EC at 20°C is measured using a Crison - Micro CM 2201. <strong>Instrumentation</strong> Spectrophotometer U-2000, Hitachi, Tokyo, Japan (N-NH4 and N-NO3) Elementar, Vario TOC, Hanau, Germany (DOC and TDN) WTW-InoLab 7110 pH-meter equipped with Hamilton GelGlass electrode (pH) Crison - Micro CM 2201 (EC)
DOI: 10.17632/wh484wfvp6.2
title: Design Neural Damper Vibration to the Improve the Stability of Electric Power Systems

description: The research of a new methodology for the Vibration damper Depends on his work on neural networks, in order to reduce the damping of electrical system and find out the
effectiveness of damper proposed in the stability of the system, so by comparing it with
traditionally Power system stabilizer, it depends on Neural network Process the signal of
rotation speed of the generator to control of the irritation synchronous machine, the
designed damper showed ability to reduce amplitude vibrations arising from failures and
thus reduce the time of damping by providing additional effort to signal entered to the
agitation system.
Characterized the proposed technical possibility of further improving the dynamic
stability and thus the stability of the electrical system
DOI: 10.17632/fm8pfvjm69.1
title: SUPPLEMENTAL MATERIAL

description: Time to onset of acne in a post hoc analysis of 3 placebo-controlled phase 3 trials of upadacitinib in patients with atopic dermatitis
DOI: 10.17632/8wzkk5mdt6.2
title: Depression and Suicidal Ideation in Mexican Medical Students Dataset

description: The data contains four attributes, sociodemographic information, depression, alcoholism, and suicide risk inventories and 247 subjects.
DOI: 10.17632/sycgz5m6dw.1
title: Biopolymer from water kefir as a potential clean-label ingredient for health applications: evaluation of new properties

description: The data showed in the documents were obtained in the evaluation of exopolysaccharide from water kefir and reflects the results for: FTIR; XRD; TG/DTG; Photostability assay; Mucoadhesion; Grain Growth. The results showed thermal and photostability, good adhesion in the porcine mucosa (TA.XT texturometer), the growth rate of the grain and also the cryopreservation of kefir grains.
DOI: 10.17632/2vfbrdxyf2.1
title: Supplementary Materials

description: Raw and Analysis of variance data of different responses associated with the figures are uploaded.
DOI: 10.17632/mtxcrx5j52.2
title: Dataset: Does the die-under-the-cup device exaggerate cheating?

description: Dataset using in Does the die-under-the-cup device exaggerate cheating?  (Antonio Alfonso et al. 2022)
DOI: 10.17632/7vrvryyghx.2
title: NMR_p66_L289K_PRE_SAXS_based_model_ver1

description: We studied structure of HIV-1 RT dimer-dissociation mutant, p66_L289K, by using Small-angle X-ray scattering (SAXS) with proton paramagnetic relaxation enhancement (PRE). Here, the data of the NMR part is stored. The SAXS part will be deposited to SAXSDB. Final structural model calculated by Xplore are also deposited here.
DOI: 10.17632/xfx39znwzp.1
title: Dataset of Leukocyte Nadir and Complete Remission Occurrence in Indonesian Acute Myeloid Leukemia Patients

description: This is a dataset of prognostic study with a retrospective cohort design. The sample was taken by total sampling from the medical record data of patients with a diagnosis of AML who were not acute promyelocytic leukemia (APL) or AML M3 FAB classification who underwent 7+3 induction chemotherapy at Dharmais Hospital National Cancer Center and Dr. Cipto Mangunkusumo National Central Public Hospital during the period from January 1st, 2015 to December 31st, 2019. The study had been approved by the local Ethics Committee. 
The acceptance criteria of this study were patients aged ≥18 years, diagnosed of AML based on at least bone marrow smear or biopsy and bone marrow aspirate or peripheral blood immunophenotyping, underwent first-line remission induction chemotherapy 7+3 regimen, and had never undergone any remission induction chemotherapy before. The criteria for rejection were AML M3 (FAB criteria) or acute promyelocytic leukemia (APL), a myeloblastic crisis phase of chronic myeloid leukemia (CML) or when the required data was not found in the patient's medical record.
The nadir leukocyte level and the time required to reach it were assessed for their associations to the occurrence of CR during the evaluation of 7+3 remission induction chemotherapy treatment. Treatment evaluations were done when the peripheral blood cells had recovered. The criteria used to define the occurrence of CR during treatment evaluation were in accordance with those established by European LeukemiaNet 2017. Factors considered as potential confounders were age, gender, AML subtype, Charlson Comorbidity Index (CCI), history of myelodysplasia syndrome (MDS), history of chemotherapy/radiotherapy, prechemotherapy leukocyte level, bone marrow myeloblast cell level at diagnosis, occurrence of febrile neutropenia and administration of granulocyte colony stimulating factor (GCSF).
DOI: 10.48370/ofd/rgc0rh
title: Sulcacis lineatocribratus (Melliié, 1849), C-449

description: Coleoptera collection
DOI: 10.48370/ofd/u9ryyu/gt35rg
title: Wyszkowski Rafał - Ryciny.pdf

description: :unav
DOI: 10.48370/ofd/u9ryyu/okkjim
title: Wyszkowski Rafał - Tabele.pdf

description: :unav
DOI: 10.48370/ofd/u9ryyu/efslg5
title: Wyszkowski Rafał.pdf

description: :unav
DOI: 10.48370/ofd/u9ryyu
title: Ocena bioróżnorodności naturalnej populacji świerka pospolitego w Puszczy Białowieskiej na podstawie analizy odnowień naturalnych tego gatunku

description: Promotor: Adolf F. Korczyk
DOI: 10.17632/36cp9kzsrf.1
title: UNMANAGED TROPICAL GREEN ROOF SPONTANEOUS VEGETATION DYNAMICS:  Effects of substrate depth

description: Data for the article "UNMANAGED TROPICAL GREEN ROOF SPONTANEOUS VEGETATION DYNAMICS: Effects of substrate depth".