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topsoil

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Series: Geological Society, London, Special Publications
Published: 28 October 2021
DOI: 10.1144/SP507-2020-49
EISBN: 9781786209948
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Journal Article
Published: 01 February 2021
Environmental & Engineering Geoscience (2021) 27 (1): 43–56.
Journal Article
Published: 01 May 2019
Environmental & Engineering Geoscience (2019) 25 (2): 169–178.
...Dimitrios Alexakis; Dimitra Gamvroula; Eleni Theofili ABSTRACT Total contents of 36 potentially toxic elements are summarized for agricultural topsoil (n = 12; soil depth = 0–20 cm), subsoil (n = 12; soil depth = 20–40 cm), and representative rock samples collected from a Mediterranean site (Megara...
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Journal Article
Published: 04 March 2019
Geochemistry: Exploration, Environment, Analysis (2019) 19 (2): 110–120.
...Jajinjav Yondonjamts; Bolormaa Oyuntsetseg; Ochirkhuyag Bayanjargal; Makiko Watanabe; Lunchakorn Prathumratana; Kyoung-Woong Kim Abstract In order to investigate copper, arsenic, lead and zinc contamination in topsoil of the Erdenet copper mining area in Mongolia, soil samples collected from...
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Journal Article
Published: 30 July 2018
Geochemistry: Exploration, Environment, Analysis (2018) 18 (4): 331–342.
...Carmela Rezza; Attila Petrik; Stefano Albanese; Annamaria Lima; Giulia Minolfi; Benedetto De Vivo Abstract This study shows the statistical and spatial distribution of Mo, Sn and W in topsoils of the Campania Region. Topsoil samples were collected based on a 16-km 2 and a 3.8-km 2 cell-sampling...
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Journal Article
Published: 30 July 2018
Geochemistry: Exploration, Environment, Analysis (2019) 19 (3): 205–215.
...Giulia Minolfi; Attila Petrik; Stefano Albanese; Annamaria Lima; Claudia Cannatelli; Carmela Rezza; Benedetto De Vivo Abstract In this paper we present a comparison of statistical and spatial distributions between Pb, Cu and Zn concentration data and clr-transformed data of 3669 topsoil samples...
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Journal Article
Published: 10 May 2018
Geochemistry: Exploration, Environment, Analysis (2018) 18 (4): 319–330.
...Attila Petrik; Stefano Albanese; Annamaria Lima; Gyozo Jordan; Roberto Rolandi; Carmela Rezza; Benedetto De Vivo Abstract Digital image processing analysis was carried out on As in topsoils of the Campania Region (Italy) to recognise any unknown spatial patterns. The highest As concentration...
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Journal Article
Published: 01 June 2016
Vadose Zone Journal (2016) 15 (6): vzj2015.11.0143.
...Maxim Poltoradnev; Joachim Ingwersen; Thilo Streck Abstract The topsoil water content (SWC) plays a key role in partitioning energy and water fluxes at the land surface. Knowledge about its spatial and temporal variability is crucial for improving climate and hydrology modeling. We investigated SWC...
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Series: GSA Special Papers
Published: 01 May 2016
DOI: 10.1130/2016.2520(17)
Series: GSA Special Papers
Published: 01 May 2016
DOI: 10.1130/2016.2520(21)
Journal Article
Published: 07 March 2016
Geochemistry: Exploration, Environment, Analysis (2016) 16 (2): 159–163.
.... Total REE concentrations (ΣREE) recorded moderate seasonal variation, ranging from 31.0 mg kg −1 to 88.2 mg kg −1 , with an average of 53.5 mg kg −1 , similar to the ΣREE of local topsoil. The values of ΣREE were negatively correlated with the corresponding dust deposition fluxes, which may be due...
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Journal Article
Published: 01 February 2016
Environmental & Engineering Geoscience (2016) 22 (1): 37–52.
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Journal Article
Published: 01 October 2015
Vadose Zone Journal (2015) 14 (10): vzj2015.05.0072.
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Journal Article
Published: 03 July 2015
Geochemistry: Exploration, Environment, Analysis (2015) 15 (4): 361–372.
...A. Cosenza; A. Lima; R. A. Ayuso; N. K. Foley; S. Albanese; A. Messina; B. De Vivo Abstract This investigation focused on topsoils ( n = 122) and vertical profiles ( n = 6) distributed over an area of 250 km 2 in the eastern-central Peloritani Mountains, northeastern Sicily. Georeferenced...
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Journal Article
Published: 01 November 2014
Vadose Zone Journal (2014) 13 (11): vzj2014.07.0089.
... surface N 2 O flux is dependent on the soil’s D p / D o , and WFPS alone does not suffice to discriminate between N 2 O emission sources. Consequently, the soil surface N 2 O flux may be comprised of N 2 O originating from deeper soil layers transported upward and/or from production in the topsoil...
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Journal Article
Published: 01 July 2014
Vadose Zone Journal (2014) 13 (7): vzj2013.09.0167.
... in agricultural soils with contrasting properties. Eighty-seven agricultural topsoils were sampled throughout Europe. Soil solution was isolated by centrifugation (3500 g) from soils sampled field moist and analyzed directly ( n = 30), from air-dried soils that were rewetted and incubated for 5 wk ( n = 30...
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Journal Article
Published: 01 June 2014
Journal of Environmental and Engineering Geophysics (2014) 19 (2): 87–99.
... is a minimum, i.e., the frequency at which particle motion is predominantly vertical and where the HVSR spectrum presents a minimum. A 10-m thick soft topsoil layer induces a resonance frequency of 9 Hz (H/V maximum) and a clear osculation frequency between modes at 13 Hz (H/V minimum). When the thickness...
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Journal Article
Published: 01 November 2013
Vadose Zone Journal (2013) 12 (4): vzj2012.0201.
... soil water content (AWC) was calculated as the difference between volumetric soil water content at field capacity (FC) and wilting point (WP). The HYPRESS topsoil pedotransfer functions ( Wösten et al., 1999 ) were chosen to estimate FC and WP, as they provided the best fit when compared to other...
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Journal Article
Published: 01 November 2013
Vadose Zone Journal (2013) 12 (4): vzj2013.02.0047.
... of observed values) and the coefficient of variation of the RMSE (CV RMSE = RMSE normalized to the mean of observed values) are also given. The two-dimensional (topsoil) spatial distribution of total sand contents in spoil heaps was characterized for both soil raster points (based on samples from the upper 30...
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Journal Article
Published: 01 November 2013
Vadose Zone Journal (2013) 12 (4): vzj2013.05.0079.
... types. The experimental method was similar to that described by Todman et al. (2013) with one major difference: the length of the experiment was significantly longer (110 vs. 10 d). The same three soil types were used: silica sand, garden topsoil, and saline sand. The saline sand was identical...
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