<i>DIVISION OF ENVIRONMENTAL SCIENCES</i>: CLAY MINERALS AND MICROBIAL ECOLOGY*,†

Stotzky, G.

doi:10.1111/j.2164-0947.1967.tb02449.x

Cited by 41 publications

(1 citation statement)

References 21 publications

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“…p5.l24: soil class cannot solely represent all the physical and chemical characteristics of conditions which influence the soil DOC concentration. You must include environmental parameters such as soil moisture (DeLuca, 1992;Kalbitz, 2000;Lundquist, 1999;Michalzik, 2001), temperature (Michalzik, 1999;Moore, 2008;Raymond, 2010), pH (Fröberg, 2011;Scheel, 2008), C:N and N effect (Gödde, 1996;Kindler et al, 2011) and soil texture (Davidson et al, 2006;Filip, 1971;Sollins, Homann, & Caldwell, 1996;Stotzky, 1967;Vogel et al, 2015) to have a realistic representation of DOC. p5.l26: You can find HWSD product which reports SOC directly (Nachtergaele et al, 2010).…”

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confidence: 99%

Comments on ‘Global database and model on dissolved carbon in soil solution’ by Joep Langeveld et al.

Anonymous

2019

Preprint

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The authors present a database which they compiled for soil dissolved organic and inorganic carbon alongside a regression model to calculate top and sub soil DOC concentration. I find the paper poorly written and organised and the model is not well constructed, missing major parameters controlling soil DOC. While I appreciate the effort of data collection which could be useful for model evaluation, I do not find model outputs and analyses reliable and do not recommend publishing this manuscript in Biogeosciences in the present format. Major comments: The main problems that I see with this manuscript are as follows: Authors constructed a model based on oversimplified parameters which are not fully representative of the processes that are controlling soil DOC. Additionally, they did not use a proper climate C1 BGD

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Section: Interactive Commentmentioning

confidence: 99%

Comments on ‘Global database and model on dissolved carbon in soil solution’ by Joep Langeveld et al.

Anonymous

2019

Preprint

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Effects of substrate mineralogy on the biodegradability of fuel components

Apitz

Meyers-Schulte²

1996

Enviro Toxic and Chemistry

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Abstract-Experiments were carried out to determine the effects of mineralogy on the biodegradability of components of a whole fuel by a soil microbial consortium. Samples of quartz sand (Fischer Sea Sand) and illite clay (API 35) were spiked with marine diesel fuel, aged, slurried, and inoculated, and concentrations of fuel components were monitored over time. To help distinguish biotic from abiotic processes, identical samples were poisoned with mercuric chloride and were run in parallel. While there was chromatographic and biomarker evidence of n-alkane biodegradation in the sand samples, illite samples showed no evidence of biogenic loss of aliphatic components. Polycyclic aromatic hydrocarbons, on the other hand, were lost equivalently on both minerals and in both cases were lost to a much greater extent than were total petroleum hydrocarbons (TPHs). These results suggest that under our experimental conditions, illite inhibited the bioavailability of some TPH components to the soil microbial consortium.

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Einfluß von Tonmineralien auf das Verhalten von acidophilen Thiobacillus‐Arten in Suspensionen

1979

J of Basic Microbiology

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DIVISION OF ENVIRONMENTAL SCIENCES: CLAY MINERALS AND MICROBIAL ECOLOGY*,†

Cited by 41 publications

References 21 publications

Comments on ‘Global database and model on dissolved carbon in soil solution’ by Joep Langeveld et al.

Comments on ‘Global database and model on dissolved carbon in soil solution’ by Joep Langeveld et al.

Effects of substrate mineralogy on the biodegradability of fuel components

Einfluß von Tonmineralien auf das Verhalten von acidophilen Thiobacillus‐Arten in Suspensionen

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