ライフサイエンスコーパス: organic matter

1 oxy of water retention capacity and sediment organic matter).

2 ates [(OH)2MgO2CR](-), in meteoritic soluble organic matter.

3 te and water were added together with labile organic matter.

4 t with that reported for terrigenous natural organic matter.

5 ide) and subsequently with diverse dissolved organic matter.

6 n and energy source rather than on dissolved organic matter.

7 the triplet states of chromophoric dissolved organic matter.

8 rough accumulation of inorganic sediment and organic matter.

9 ysis of photooxidants generated by dissolved organic matter.

10 mulation at increased availability of labile organic matter.

11 enzymatic Fenton-based decomposition of soil organic matter.

12 about physicochemical stabilization of soil organic matter.

13 n solution, cationic polymers, and suspended organic matter.

14 bout factors regulating the turnover of soil organic matter.

15 cal to the preservation of soil and sediment organic matter.

16 ossible repositories for the preservation of organic matter.

17 ution with increased salinity than dissolved organic matter.

18 ted by the sediment's content of particulate organic matter.

19 ute to the daily flux of billions of tons of organic matter.

20 are the main precursor of mineral-associated organic matter.

21 uranium retention and the essential role of organic matter.

22 rived from heterotrophic remineralization of organic matter.

23 the cycling of nutrients through decomposing organic matter.

24 crobial communities associated with decaying organic matter.

25 ecause it is isotopically district to marine organic matter.

26 has an essential role in the manipulation of organic matter.

27 il, as well as free and occluded particulate organic matter.

28 , ionic strength (0.001-0.1 M) and dissolved organic matter (0-20 mg L(-1)), making it suitable for a

29 attach to, and use patches of nutrients and organic matter (2,3) .

30 ter have accumulated in occluded particulate organic matter ( 20%; oPOM); however, experimental N dep

31 Excited triplet state chromophoric dissolved organic matter ((3)CDOM*) is a short-lived mixture of ex

32 reactive species, such as triplet dissolved organic matter ((3)DOM) and singlet oxygen ((1)O2), cont

33 triplet excited states of dissolved natural organic matter ((3)DOM*) and the efficiency of (3)DOM* f

34 included triplet excited states of dissolved organic matter ((3)DOM*), singlet oxygen ((1)O2), and th

35 ith a marked impact on the depletion of soil organic matter, a signature property of mollisols.

36 inputs of bacterial detritus, and bacterial organic matter accounted for 21-42% of DOC in all waters

37 an reside in soils for decades to centuries, organic matter accumulating under future rates of anthro

38 g surface chemistries and to three dissolved organic matter adlayers, as a function of solution pH an

39 varying crystallinity or impurities such as organic matter, Al or Si, persisted under suboxic-oxic c

40 contrasted properties: a sandy soil poor in organic matter and a clay soil rich in organic matter, b

41 nsight into the accessibility of sedimentary organic matter and demonstrate how bioavailability of na

42 Finally, in vitro organic matter and dry matter digestibility were assesse

43 kes comparative analysis of crop yield, soil organic matter and economic benefits within the practice

44 (II)-thiolate complexes (Hg(SR)2) in natural organic matter and in cysteine solutions was demonstrate

45 his signature is characteristic of aliphatic organic matter and is mainly localized on a broad region

46 Interactions between organic matter and mineral matrices are critical to the

47 forearc (Pacific Ocean) that contain complex organic matter and nanosized Ni-Fe alloys.

48 cosystem processes and attributes, including organic matter and nutrient cycling, marsh-estuarine foo

49 In the silt loam sediment with abundant organic matter and nutrients, the decay rates of both is

50 onAMF) access to a compartment containing an organic matter and soil patch in two independent microco

51 The depletion of most natural dissolved organic matter and the fact that an extensive mobilizati

52 Particulate organic matter and total soil C declined over time in al

53 (N2-fixation), modified herbivory (sediment organic matter and water content), or their interaction

54 ECM fungi have the capacity to decompose organic matter, and although there is increasing evidenc

55 ay critical roles on the degradation of soil organic matter, and measurements of their activities are

56 streams were abundant in chlorophylls, fresh organic matter, and organic nitrogen, whereas in winter,

57 was amended 16 years ago with process sand, organic matter, and seeded (partially treated), and a th

58 O2, turbidity, algal pigments, and dissolved organic matter are now enabling observations of watershe

59 chemical similarities to abiotic meteoritic organic matter) are relatively resistant.

60 obes rely largely on solubilized particulate organic matter as a carbon and energy source rather than

61 Rechargeable batteries that use organic matter as the capacity-carrying material have pr

62 e type, surface, pre-cleaning practices, and organic matter, as an efficacious measure to interrupt d

63 For example, riverine organic matter assimilation by the glacier-nesting seabi

64 determination of the chemical nature of the organic matter associated with phytoliths remains a chal

65 plants may potentially influence the fate of organic matter associated with soil mineral and aggregat

66 ovides a more detailed understanding of soil organic matter at the molecular level itself key to deve

67 caused by a switch in motility attributed to organic matter availability.

68 ammonium and phosphate when biochar derived organic matter (BDOM) was included.

69 Hydraulic conductivity, nutrients and organic matter, biofilm biomass, and activity were analy

70 or in organic matter and a clay soil rich in organic matter, both contaminated with 1, 15, and 50 mg.

71 al transport of PFASs due to the settling of organic matter bound PFAS (biological pump) was estimate

72 We hypothesise that reductions in organic matter brought about by litter removal may lead

73 xia would have resulted in elevated rates of organic matter burial that would have acted as an additi

74 by the mineralisation of different types of organic matter buried in the sediment.

75 They feed and breed in fecal and decaying organic matter, but the microbiome they harbour and tran

76 l N deposition has fostered the occlusion of organic matter by mineral soil particles, our results hi

77 availability influences the decomposition of organic matter by soil microbial communities.

78 Natural organic matter can be an additional silver sink in envir

79 of 1984-1988 to 2004-2008, the national dead organic matter carbon stock has increased by 6.7 +/- 2.2

80 optical properties of chromophoric dissolved organic matter (CDOM) and humic substances (HS) remains

81 Marine chromophoric dissolved organic matter (CDOM) and its related fluorescent compon

82 at the Fe L3 and C K1 edges showing that the organic matter co-localized with Fe(III) consists primar

83 n OC and iron, as well as the composition of organic matter co-localized with ferric iron.

84 hnologies and high rates and independence of organic matter compared to bioelectrochemical systems.

85 rrihydrite, gibbsite, and/or Fe(III)-natural organic matter complexes and V(4+) in the structure of g

86 ivalent static column system over a range of organic matter concentrations and ionic strengths.

87 de, and benzophenone) at different dissolved-organic-matter concentrations, which change the overall

88 d Raman spectroscopy, we determined that the organic matter consists of a mixture of aliphatic and ar

89 trients were associated with changes in soil organic matter content and quality (carbon to nitrogen r

90 les and hence reduced Ce uptake, whereas the organic matter content enhanced Ce uptake.

91 vegetation (peat defined as material with an organic matter content of at least 65 per cent to a dept

92 e impact of soil properties (textural class, organic matter content) and the presence of hydrocarbon

93 r content and low total nitrogen, carbon and organic matter content.

94 The efficiency by which fungi decompose organic matter contributes to the amount of carbon that

95 systems play significant roles in degrading organic matter, controlling diseases, and formation of a

96 ming results in a four-phase pattern of soil organic matter decay and carbon dioxide fluxes to the at

97 oth observations and models show that high N organic matter decomposes more rapidly.

98 e from shales in hydraulic fracture systems, organic matter decomposition in soil, weathering and soi

99 Incorporations of experimental results into organic matter decomposition models suggest that paramet

100 ecosystems where primary production exceeds organic matter decomposition rates in the soil, and ther

101 veground net primary productivity (ANPP) and organic matter decomposition, and combined those data wi

102 e-to-fine grain sizes promoted a hot-spot of organic matter degradation and biomass growth at the int

103 r diverse microbial communities that mediate organic matter degradation and influence biogeochemical

104 C m(-2) yr(-1) ) and isotope composition of organic matter (delta(13) CTOC ).

105 Nutrients and organic matter distribution in depth influence physicoch

106 of climate and stand characteristics on dead organic matter distribution.Reliable estimates of the to

107 Sites of dissolved organic matter (DOM) accumulation could promote the mixo

108 Natural dissolved organic matter (DOM) affects mercury (Hg) redox reaction

109 omplex mixtures of natural aquatic dissolved organic matter (DOM) and compared this technique to the

110 ces to induce cascading effects on dissolved organic matter (DOM) and microbial communities in the su

111 Specifically, the effects of dissolved organic matter (DOM) and sediment on SPM-MWCNTs under va

112 II)) in aquatic systems containing dissolved organic matter (DOM) and sulfide is necessary to predict

113 d focus on nitrogen (N)-containing dissolved organic matter (DOM) as a nutrient source supporting eut

114 the presence of negatively charged dissolved organic matter (DOM) as coadsorbate remains poorly studi

115 ar size plays an important role in dissolved organic matter (DOM) biogeochemistry, but its relationsh

116 amazepine (CBZ) in the presence of dissolved organic matter (DOM) by Fourier transform ion cyclotron

117 reassessed the molecular weight of dissolved organic matter (DOM) determined by high pressure size ex

118 synthetic water samples containing dissolved organic matter (DOM) extracts and bromide were treated u

119 transfer of terrestrially derived dissolved organic matter (DOM) from land to surface waters.

120 natural aquatic systems scavenges dissolved organic matter (DOM) from solution.

121 ntibiotics in solutions containing dissolved organic matter (DOM) from three poultry litter extracts

122 The quality of dissolved organic matter (DOM) in a wet weather overflow (WWF) can

123 lays an important role in altering dissolved organic matter (DOM) in estuarine and coastal sediments,

124 ize origins and transformations of dissolved organic matter (DOM) in five major Arctic rivers (Kolyma

125 Dissolved organic matter (DOM) in the oceans is one of the largest

126 tential abiotic transformations of dissolved organic matter (DOM) in the water column.

127 d that the chemical composition of dissolved organic matter (DOM) leached from the sand patties under

128 Wildfires can elevate dissolved organic matter (DOM) levels due to ash input and algal g

129 Dissolved organic matter (DOM) negatively impacts granular activat

130 Dissolved organic matter (DOM) quantity and composition control th

131 Dissolved organic matter (DOM) strongly influences the properties

132 was faster in solutions containing dissolved organic matter (DOM) than in ultrapure water, illustrati

133 nge is accelerating the release of dissolved organic matter (DOM) to inland and coastal waters throug

134 exchange between iron and dissolved natural organic matter (DOM) were not substantially influenced b

135 Reactions of dissolved organic matter (DOM) with aqueous sulfide (termed sulfur

136 amine the molecular composition of dissolved organic matter (DOM) within these lakes using Fourier tr

137 ontent and speciation of sulfur in dissolved organic matter (DOM), which influences the reactivity of

138 ydroxyl radical ((*)OH) present in dissolved organic matter (DOM).

139 oduction and discharge of reactive dissolved organic matter (DOM).

140 of the composition of fluorescent dissolved organic matter (DOM).

141 king due to insufficient information on dead organic matter (DOM).

142 and is an important repository of dissolved organic matter (DOM).

143 terise the chemical composition of dissolved organic matter (DOM).

144 el of humic-like and nonhumic-like dissolved organic matter (DOM).

145 er understanding of the occurring changes of organic matter during ozonation.

146 especially when combined with nutrient-rich organic matter, e.g., co-composted biochar.

147 arbon and nitrogen isotope analyses of total organic matter (expressed as delta(13)C and delta(15)N v

148 ted with leaf litter, wood, and fine benthic organic matter (FBOM) across seasonal temperature gradie

149 f a definite mineral assemblage with various organic matter forms and a specific pore system, each fu

150 The rich diversity and complexity of organic matter found in meteorites is rapidly expanding

151 ties of silt and clay particles that occlude organic matter from microbial attack.

152 Contaminated soil organic matter from the Rocky Flats Environmental Techno

153 ur quantitative abilities to model important organic matter functions such as metal complexation and

154 lts on biotic factors further suggested that organic matter gains or losses induced the observed stru

155 chloride or most additions including labile organic matter (glucose and maltose).

156 l abrupt changes in lithology, percent total organic matter, grain size, and magnetic susceptibility.

157 was amended 16 years ago with process sand, organic matter, gypsum, and seeded (fully treated), anot

158 ations suggest that biochemically equivalent organic matter has accumulated in oPOM at a greater rate

159 Although organic matter has been detected at Gale Crater, Mars, i

160 The microbial contribution to soil organic matter has been shown to be much larger than pre

161 adation, the photochemical mineralization of organic matter, has been recently identified as a mechan

162 Significant amounts of organic matter have accumulated in occluded particulate

163 Long residence times of soil organic matter have been attributed to reactive mineral

164 These reactions between sulfide and organic matter have important implications for our under

165 m, which we attribute to low connectivity of organic matter-hosted and clay-associated pores in these

166 (FLU), but also salicylic acid (SA), natural organic matter (humic acid, HA), and dissolved silicates

167 ctivity combined with sinking photosynthetic organic matter in a soft-sediment setting creates geoche

168 ven the increasing prevalence of terrigenous organic matter in aquaculture feed stocks because it is

169 s one of several mechanisms by which natural organic matter in aquatic and soil environments may play

170 related to the concentration of terrestrial organic matter in experiments or lakes, but rather to th

171 For the anaerobic remineralization of organic matter in marine sediments, sulfate reduction co

172 Organic matter in permeable sediments is dominated by mi

173 Recycling of organic matter in sediments is an important component of

174 nhancing the processing and turnover of dead organic matter in soils of arid regions), reduce human e

175 The degradation of organic matter in the anoxic seabed proceeds through a c

176 xplanation for the origin of sulfur-depleted organic matter in the deep ocean and cannot adequately r

177 most rapid heterotrophic transformations of organic matter in the environment.

178 e-of-flight mass spectrometer) and dissolved organic matter in the ocean point to a marine source for

179 cquiring nitrogen, all species converted the organic matter in the SOM extract using oxidative mechan

180 surements of the (15)N/(14)N of fossil-bound organic matter in the stony deep-sea coral Desmophyllum

181 5, and its association with increased pH and organic matter in two protected surface water supplies (

182 However, the presence of dissolved organic matter in water enhanced particle stability and

183 To examine a possible role in fouling from organic matter in water, cathodes were exposed to high c

184 ight play a significant role in metabolising organic matters in the PRE and other temperate estuarine

185 ailable information on carbon stocks in dead organic matter, including woody debris and litter, reduc

186 The optical properties of dissolved organic matter influence chemical and biological process

187 ent associated with forest fertilization and organic matter influx which may have facilitated growth

188 Stability of this fresh organic matter input to surface soil is unknown, but is

189 enerally only a small component of the total organic matter inputs to the food web, even in the most

190 lake waters with high terrestrial dissolved organic matter inputs.

191 Additionally, added organic matter interfered with particle growth on the fa

192 nd (COD) and recovered up to 55% of incoming organic matter into sludge.

193 ge enrichments in deuterium of the insoluble organic matter (IOM) isolated from the carbonaceous mete

194 zones (NRZs) containing sediments higher in organic matter, iron sulfides, and non-crystalline U(IV)

195 Natural chlorination of organic matter is common in soils.

196 oversimplified view that remineralization of organic matter is the major pathway releasing DFe throug

197 the absorbance and fluorescence response of organic matter isolates to changes in solvent temperatur

198 ostly from soaps and detergents as dissolved organic matter, its fate can be selectively determined d

199 solids; however, in the presence of natural organic matter, lead oxide dissolution was 36 times grea

200 zone attack on resins, asphaltenes, and soil organic matter led to the production of NO3(-), SO4(2-),

201 otroph to remineralize the inevitably leaked organic matter, making nutrients circulate in a mutualis

202 Dissolution of adsorbates into organic matter may also affect the hysteresis.

203 e, we use the recently developed Vienna Soil Organic-Matter Modeler to create representative models o

204 eld parameters, available at the Vienna Soil Organic-Matter Modeler.

205 s of molecular weight-fractionated dissolved organic matter (MW-fractionated DOM) in the catchment an

206 gradients of pH, ionic strength, and natural organic matter (NOM) concentrations.

207 rces are weakened by the presence of natural organic matter (NOM) conditioning films, owing to the hy

208 Addition of natural organic matter (NOM) did not significantly impact pSi's

209 aling inhibitors hinder clogging but natural organic matter (NOM) has relatively little impact.

210 Natural organic matter (NOM) is capable of interfering with Fe h

211 values (6.3-7.5) and three types of natural organic matter (NOM) isolates at various concentrations

212 l-complexing ligands associated with natural organic matter (NOM) often prevents the formation of iro

213 operties induced by interaction with natural organic matter (NOM) warrant consideration in assessing

214 ents at 5 mgC.L(-1) and 50 mgC.L(-1) natural organic matter (NOM), 10(-9)-10(-10) M (238)Pu, and 0.1

215 ols and thiol groups associated with natural organic matter (NOM), as determined by sulfur K-edge X-r

216 ted elemental formula assignment for natural organic matter (NOM).

217 ngly influenced by complexation with natural organic matter (NOM).

218 s spectrometry (FTICR MS) studies of natural organic matter (NOM).

219 e presence or absence of sulfide and natural organic matter (NOM, as humic acid), while under suboxic

220 Fe to remain in suspension interactions with organic matter (OM) are fundamental and these interactio

221 for describing the apparent kinetics of bulk organic matter (OM) decomposition.

222 esidue and apple wood combustion were mainly organic matter (OM) in smoldering phase, whereas soot-OM

223 curs in the presence of mineral sorbents and organic matter (OM) in soils and sediments; however, thi

224 nitude greater in pyroclastic materials with organic matter (OM) inputs relative to those without, de

225 Organic matter (OM) plays a major role in both terrestri

226 Solid organic matter (OM) plays an essential role in the gener

227 ial ecosystems and their vegetation and soil organic matter (OM) pools is often non-linear and poorly

228 ed studies of their rates of accumulation of organic matter (OM), organic carbon (OC) and total nitro

229 7 wt % C), and As- (1280 and 1230 mg/kg) and organic matter (OM)-rich (18.1 and 21.8 wt % C) freshwat

230 The four contrasting sorbents included an organic matter (OM)-rich peat soil, an OM-poor clay soil

231 but the influence of the influx of riverine organic matter on the trophodynamics of coastal marine f

232 of the charge-transfer model for explaining organic matter optical properties and suggest that futur

233 Dissolved organic matter optical properties have been attributed t

234 efficiency were the soil properties; a high organic matter or clay content was observed to negativel

235 ements with a particularly high affinity for organic matter or oxides.

236 rized from soils amended with three types of organic matter over a 30-year fertilization experiment.

237 take, but not significantly affected by soil organic matters, pH or the other four heavy metals (Cr,

238 ch should explore other models for dissolved organic matter photophysics.

239 tal dynamics around an aggregate of reactive organic matter placed on the SWI of a sediment mesocosm.

240 Deposition of particulate organic matter (POM) induces diagenetic hot spots at the

241 By identifying which compounds of the organic matter pool are absorbed, transported, and incor

242 ate that the sequestered Hg is bound in soil organic matter pools accumulating over millennia.

243 at is, C fluxes from live vegetation to dead organic matter pools.

244 ronitrobenzene (4-ClNB) as a function of pH, organic matter presence, and reactant concentrations was

245 leave organic groups and hydrolase polymeric organic matter produced by the cyanobacterium.

246 munities responded to the seasonal shifts in organic matter quality and chemical composition.

247 ity in phytoplankton classes, herbivory, and organic matter quality in a freshwater river network.

248 zation and aromaticity, suggesting that soil organic matter quality is an important parameter affecti

249 ies through their direct effect on dissolved organic matter quality, while saprotrophic fungi directl

250 me activity, respiration rates, and residual organic matter reactivity.

251 that the dominant DFe sources are linked to organic matter remineralization, either in the water col

252 However, we find that enhanced burial of organic matter seems to have been important in eventuall

253 PFAS (biological pump) was estimated from an organic matter settling fluxes climatology and the PFAS

254 o permit a semi-quantitative analysis of the organic matter, showing the presence of peptides and car

255 Soil organic matter (SOM) and the carbon and nutrients therei

256 ce soils, and the ability to chlorinate soil organic matter (SOM) appears widespread among microorgan

257 key importance, given the relevance of soil organic matter (SOM) as a vast C pool and climate change

258 zymatic liberation of nitrogen (N) from soil organic matter (SOM) has recently been invoked as a key

259 elevation as pH decreased (6.2-4.4) and soil organic matter (SOM) increased (18-157 mg C g(-1) ).

260 cquisition model with a microbe-focused soil organic matter (SOM) model.

261 Soil organic matter (SOM) supports the Earth's ability to sus

262 communities in driving the responses of soil organic matter (SOM) to multiple management practices.

263 climatic influences on the formation of soil organic matter (SOM).

264 reducing the decay of plant litter and soil organic matter (SOM).

265 play a central role in the breakdown of soil organic matter (SOM).

266 marine consumers, estimates of the riverine organic matter source contribution to upper trophic-leve

267 ) C) isotopes that trace riverine and marine organic matter sources as they are passed from lower to

268 e food webs were primarily composed of young organic matter sources released from glacier ecosystems

269 Suwannee River natural organic matter (SRN) was used as a surrogate DOM standar

270 ulvic acid (SRFA) and Suwannee River natural organic matter (SRNOM), LDI was found to ionize a very s

271 g insights into factors responsible for soil organic matter stabilization and decomposition are being

272 y- to millennia-old carbon from the peatland organic matter stock.

273 ounterbalance is effected by modulating soil organic matter stocks.

274 Most of the organic matter stored in these systems is in soils where

275 The effect that labile organic matter strongly stimulated the chlorination rate

276 quantified the ecological impact of riverine organic matter subsidies to glacier-marine habitats by d

277 eral surfaces (goethite and gamma-Al2O3) and organic matter [Suwannee River fulvic acid (SRFA)] on Fe

278 l soil-with consistent stimulation by labile organic matter that did overrule the negative effects of

279 fected by humic acid, a component of natural organic matter that fouls activated carbons.

280 Moreover, in the soil poor in organic matter, the organic citrate coating significantl

281 sea ice productivity and reduced delivery of organic matter to the benthos driven by recent warming i

282 Aquatic ecosystems depend on terrestrial organic matter (tOM) to regulate many functions, such as

283 predicting the factors controlling iron and organic matter transformation and bioavailability in aqu

284 to microbial cells, intriguing insights into organic matter transformation in the deep ocean emerged.

285 e relative proportions of gaseous C loss and organic matter transport downstream should not change wi

286 ssure whereas aromatic hydrocarbon-dominated organic matter types (types III and IV; mainly land plan

287 reveal that long chain hydrocarbon-dominated organic matter (types I and II; mainly microbial or alga

288 rmed by the build-up of partially decomposed organic matter under waterlogged anoxic conditions.

289 to total organic C ratio indicates that soil organic matter was used more efficiently by microbes col

290 between orthophosphate and water-extractable organic matter (WEOM) for adsorption to iron (oxy)hydrox

291 s of thermal-alteration on water extractable organic matter (WEOM), soil samples were heated in a lab

292 ich was relatively enriched in nutrients and organic matter, were primarily water-limited, compared w

293 lyzing atmospheric submicrometer particulate organic matter which combines direct particle sampling a

294 er variables, such as pH and the presence of organic matter, which could lead to the evolving reactiv

295 e in the (15)N/(14)N of coral skeleton-bound organic matter, which signals increased deposition of an

296 beling of cyanobacterially derived dissolved organic matter with advanced two-dimensional NMR spectro

297 ctra enabled monitoring of multiple types of organic matter with different O3 and HO(*) reactivity.

298 microbes in bare land soils also faced soil organic matter with the high ratio of recalcitrant C to

299 em health, must consider U(IV) adsorption to organic matter within the sediment environment.

300 e average amount of evaporated water-soluble organic matter (WSOM = WSOC x 1.95) was 0.6 mug m(-3); h