Influence of Humic Acid on Sorption of Neptunium(V) onto Soil

1994 ◽  
Vol 353 ◽  
Author(s):  
Y. Sakamoto ◽  
S. Nagao ◽  
T. Ohnuki ◽  
M. Senoo ◽  
A. Ohashi ◽  
...  

AbstractThe pH dependence of the stability constant of Np(V)-humate and the sorption of Np(V) onto soil was studied to clarify the influence of dissolved organic carbon on the migration behavior of Np(V) in soil layer. The stability constant of Np(V)-humate was expressed by logβ1=(0.35 ±0.03)pH+0.04±0.01 in the pH region from 5.3 to 8.7, and the intrinsic stability constant by logβ*1=3.66±0.05.The sorption of Np(V) increased with pH up to pH 7, and tended to reach maximum, about 95%, at pH 9 in the absence of humic acid. In the presence of humic acid more than 140mg/l, the sorption of Np(V) was lower than that in the absence of humic acid above pH 7, while any influence of humic acid on the sorption of Np(V) onto soil was not observed below pH 7. The sorption behavior of Np(V) onto soil was explained by reversible sorption of NpO2+ and sorption of NpO2CO3- and/or NpO2OH. Further, the influence of the size distribution of Np(V) on the sorption onto soil was examined and discussed.

1986 ◽  
Vol 84 ◽  
Author(s):  
J.I. Kim ◽  
G. Buckau ◽  
W. Zhuang

AbstractThe generation of humic colloids of Am(III) has been investigated in Gorleben groundwaters containing different amounts of humic substances. Dissolved organic carbon (DOC) in these groundwaters consists mainly of humic acid and fulvic acid, which is present in a colloidal form through aggregation with trace heavy metal ions of groundwater constituents. Concentrations of these heavy metal ions are proportional to the DOC concentration. The generation of Am(III) pseudocolloids through geochemical interactions with humic colloids in different groundwaters is quantified by ultrafiltration as well as ultracentrifugation by the aid of radiometric concentration measurements. The speciation of dissolved Am(III) species in groundwaters is carried out by laser induced photoacoustic spectroscopy (LPAS).


2015 ◽  
Vol 2 (3) ◽  
pp. 280-287 ◽  
Author(s):  
Joris J.-H. Haftka ◽  
Patrick S. Bäuerlein ◽  
Erik Emke ◽  
Nienke Lammertse ◽  
Daria Belokhovstova ◽  
...  

Influence of various parameters on the stability and size of fullerene clusters is being investigated using DLS, MALS and flow cytometry.


1999 ◽  
Vol 79 (2) ◽  
pp. 321-324 ◽  
Author(s):  
T. R. Moore ◽  
L. Matos

We examined the influence of dissolved organic carbon (DOC) source on the sorption of DOC by two clayey and two sandy soils using seven extracts from plant tissues and organic soil horizons. Sorption characteristics, such as null-point DOC concentration, partition coefficient and intercept, were determined over the initial solution concentration range of 0–50 mg DOC L−1. The clayey soils had larger partition coefficients and higher null points than the sandy soils. There was an average threefold variation in null-point DOC concentration and partition coefficient amongst the seven DOC extracts. Fractionation of the DOC samples into humic acid and hydrophobic and hydrophilic acids, bases and neutrals revealed weak relationships between the sorption characteristics and DOC chemistry. Key words: Dissolved organic carbon, sorption, fractionation, humic acid, fulvic acid


2005 ◽  
Vol 35 (9) ◽  
pp. 2130-2140 ◽  
Author(s):  
A S Prokushkin ◽  
T Kajimoto ◽  
S G Prokushkin ◽  
W H McDowell ◽  
A P Abaimov ◽  
...  

Fluxes of dissolved organic carbon (DOC) in forested watersheds underlain by permafrost are likely to vary with changes in climatic regime that increase soil moisture and temperature. We examined the effects of temporal and spatial variations in soil temperature and moisture on DOC fluxes from the forest floor of contrasting north- and south-facing slopes in central Siberia. DOC fluxes increased throughout the growing season (June–September) on both slopes in 2002 and 2003. The most favorable combination of moisture content and temperature (deepest active soil layer) occurred in September, and we believe this was the primary driver of increased DOC concentrations and flux in autumn. Total DOC flux for June–September was 12.6–17.6 g C·m–2 on the south-facing slope and 4.6–8.9 g C·m–2 on the north-facing slope. DOC concentrations in forest floor leachates increased with increasing temperature on the north-facing slope, but were almost unaffected by temperature on the south-facing slope. Our results suggest that water input in midseason from melting of ice or precipitation events is the primary factor limiting DOC production. Significant positive correlations between amounts of precipitation and DOC flux were found on both slopes. Dilution of DOC concentrations by high precipitation volumes was observed only for the forest floor leachates collected from the north-facing slope. Our results suggest that global warming will result in increased DOC production in forest floors of permafrost regions, and that precipitation patterns will play an important role in determining the magnitude of these changes in DOC flux as well as its interannual variability. However, the longer-term response of soils and DOC flux to a warming climate will be driven by changes in vegetation and microbial communities as well as by the direct results of temperature and moisture conditions.


1988 ◽  
Vol 20 (3) ◽  
pp. 55-59 ◽  
Author(s):  
Z. Filip ◽  
R. Smed-Hildmann

Humic substances account for the main part of the dissolved organic carbon in groundwater. Since groundwater aquifers located near to sanitary landfills usually contain higher concentrations of dissolved organic carbon, we made experiments in the laboratory to determine whether humic substances can be formed from simple non-humified organic substances by a complex micro-flora of municipal refuse. In liquid cultures incubated for two months humic substances were produced, especially when casein or starch was added. The highest amounts of humic acid-like substances were yielded from cultures inoculated with the indigenous microflora from a rotted (aerobic) landfill. Minor yields were obtained when the inoculum originated from a compacted (anaerobic) landfill or from a five years old landfill containing refuse and sewage sludge. Spectral characteristics indicated some similarities but also differences in the UV and visible regions between the newly formed humic acids and a humic acid from groundwater.


Toxics ◽  
2021 ◽  
Vol 9 (3) ◽  
pp. 54
Author(s):  
Karsten Schlich ◽  
Cecilia Díaz ◽  
Benjamin Gomez Pizarro ◽  
Burkhard Knopf ◽  
Ruben Schlinkert ◽  
...  

Adequate functioning of a sewage treatment plant (STP) is essential to protect the downstream aquatic environment (ECHA 2017), and information on the degradability of chemicals and their toxicity to activated sludge microorganisms is required. An environmental realistic higher tier test is a STP simulation test as described in OECD 303A (2001) which for nanoparticles can also be used to study their sorption behavior to activated sludge. However, information is limited on the influence of synthetic sewage on the microbial community of the activated sludge. A modified community can result in modifications of the sludge floccules affecting the sorption behavior. The main objective of our study was to show whether a representative microbial diversity remains under standardized test conditions as described in OECD 303A (2001) using synthetic sewage as influent. Furthermore, we investigated whether just considering the functional properties of a STP (elimination of dissolved organic carbon; nitrification), is sufficient for an assessment of gold nanoparticles (AuNPs) or whether the influence on microbial diversity also needs to be considered. AuNPs were used as a case study due to their rising medical applications and therefore increasing probability to reach the sewer and STP. The results can provide significant input for the interpretation of results from the regulatory point of view. To deliver these objectives, the general changes of the microbial population in activated sludge and its influence on the degradation activity (dissolved organic carbon (DOC) and inorganic nitrogen) using freshly collected sludge from the municipal STP in an artificial test system as a model STP in accordance with OECD 303A (2001) were assessed. Additionally, we evaluated the potential impact of AuNPs and its dispersant on the microbial composition and the overall impact on the function of the STP in terms of DOC degradation and nitrogen removal to observe if an assessment based on functional properties is sufficient. The bacteria composition in our study, evaluated at a class level, revealed commonly described environmental bacteria. Proteobacteria (β, α, δ) accounted for more than 50% but also nitrifying bacteria as Nitrospira were present. Our results show that mainly within the first 7 days of an acclimatization phase by addition of synthetic sewage, the bacterial community changed. Even though AuNPs can have antibacterial properties, no adverse effects on the function and structure of the microorganisms in the STP could be detected at concentrations of increased modeled PEC values by a factor of about 10,000. Complementary to other metallic nanomaterials, gold nanomaterials also sorb to a large extent to the activated sludge. If activated sludge is used as fertilizer on agricultural land, gold nanoparticles can be introduced into soils. In this case, the effect on soil (micro)organisms must be investigated more closely, also taking into account the structural diversity.


2021 ◽  
Author(s):  
Marta Pérez-Rodríguez ◽  
Harald Biester

Abstract Understanding the role of catchment properties is crucial for anticipating soil-derived dissolved organic carbon (DOC) export to aquatic systems, especially under changing climatic conditions. We present natural variations in DOC concentrations and fluxes in eight catchments differing in size (3 – 300 km 2 ), morphology (very steep to flat), and landscape type (Patagonian steppe, forest and peatland) along a steep precipitation gradient in remote pristine southern Patagonia, Chile. Discharge, precipitation and water chemical parameters were used to differentiate the mechanisms controlling DOC release in different catchment types. The results show large differences between catchments in terms of DOC concentrations (2 - 47 mg L -1 ) and fluxes (1 to 44 tons km -2 yr -1 ) but also in response to changes in precipitation. Small steep and forested catchments are the most reactive in terms of DOC export; specifically, changes in discharge produce fast, high and exponential increases in DOC release. DOC leaching by surface run-off through the organic soil layer is the main source of DOC during high precipitation events, and steep catchments became short-term hotspots for DOC export. In the flat catchments of the Patagonian steppe, the generally lower precipitation rates favour temporal accumulation of DOC in soils, and seasonal high discharge events produce one-off increases in DOC fluxes. Although peatlands constitute a large and continuous source of DOC export, the influence of discharge variation on DOC fluxes in peatland-dominated catchments appears to be low, despite the large carbon pools. Thus, in DOC catchments with similar precipitation regimes, morphology is the dominant factor determining ecosystem responses, where the steepest catchments show the highest sensitivity to rain events in terms of DOC export. Morphology and hydrological buffer capacity rather than the size of the carbon pools or precipitation intensity determine the export of DOC from catchments during strong rain events.


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