ライフサイエンスコーパス: organic matter

1 hectare per year from the breakdown of soil organic matter.

2 the decomposition and export of preexisting organic matter.

3 sk assessment in environments low in natural organic matter.

4 ependence of [Formula: see text] in exported organic matter.

5 d reduced species richness, biomass and soil organic matter.

6 m the incomplete combustion and pyrolysis of organic matter.

7 sotope analyses of producers, consumers, and organic matter.

8 ked paradox concerning the long-term loss of organic matter.

9 chemical elements that nature uses to build organic matter.

10 of atmospheric oxidants on par with natural organic matter.

11 crease in the presence of an aquatic natural organic matter.

12 nfluenced by regional changes in sulfate and organic matter.

13 es through the production and consumption of organic matter.

14 ough the remineralization of benthic-derived organic matter.

15 of microbial necromass as part of persistent organic matter.

16 t the ecosystems they inhabit lose almost no organic matter.

17 ycorrhizal fungi to acquire carbon from soil organic matter.

18 he remineralization of high molecular weight organic matter.

19 reservoirs depends on the amount of settling organic matter.

20 deep biosphere that include the recycling of organic matter.

21 lay important roles in the cycling of marine organic matter.

22 utaries had high concentrations of dissolved organic matter (~1.8 mmol C L(-1)).

23 ere primarily through the combustion of soil organic matter(1-3).

24 ((1)O(2)) and triplet chromophoric dissolved organic matter ((3)CDOM*) are photochemically produced r

25 uently used to probe triplet-state dissolved organic matter ((3)CDOM*) reactivity, but there remain o

26 r for triplet-excited chromophoric dissolved organic matter ((3)CDOM*), an important transient specie

27 such as excited triplet states of dissolved organic matter ((3)DOM*), singlet oxygen ((1)O(2)), and

28 for Hg(2+) complexed with natural dissolved organic matter: 9.0 x 10(-6) versus 9.8 x 10(-7) cm(2) s

29 1 soil predictor variables, including pH and organic matter accounted for a small proportion of the v

30 s a model to predict the fate and quality of organic matter along a river continuum.

31 the decomposition and source of sedimentary organic matter along the river-estuary-ocean continuum.

32 tases catalyze the hydrolysis of P from soil organic matter, an important adaptive mechanism for ecos

33 hydrothermal alteration of sediments rich in organic matter and carbonates around the dikes and sills

34 on was mainly attributed to the oxidation of organic matter and ferrous iron.

35 Natural organic matter and humic substances (HS) in soils and se

36 ative of reactive phenolic groups in natural organic matter and industrial phenolic contaminants and

37 ulated degradation of previously unavailable organic matter and led to increased liberation of "old"

38 al activity, indicating a reduced storage of organic matter and microbial residues as soil C and N.

39 (C) sink is mediated by interactions between organic matter and mineral phases.

40 to unambiguously discriminate plastics from organic matter and mineral sediments, overcoming the cap

41 ctionated, compound-dependent persistence of organic matter and modulating future perturbations in mi

42 than observed in low C/N reactors (fed with organic matter and nitrogen).

43 line mineral phases in interaction with soil organic matter and represents in many cases (respectivel

44 been proposed as a means to reduce losses of organic matter and sequester soil carbon for climate cha

45 ing can accelerate the decomposition of soil organic matter and stimulate the release of soil greenho

46 winter fallow field, we found that the soil organic matter and total nitrogen of the + C treatment w

47 a higher amount of Fe and a lower amount of organic matter and U relative to the 1-3 kDa fraction.

48 naturally occurring element that bonds with organic matter and, when converted to methylmercury, is

49 Analyses of water, sediment, organic matter, and aquatic biota revealed that PFASs we

50 arine oxygen production, remineralization of organic matter, and biofilm formation.

51 s if surface-applied, strong binding to soil organic matter, and negligible leaching into water.

52 ctrolyte dilution, the addition of dissolved organic matter, and physical scouring.

53 robial respiration; and (c) decomposition of organic matter, and sampled communities of aquatic fungi

54 xtracellular enzymes are master recyclers of organic matter, and to predict their functional lifetime

55 y particle settling, binding of MeHg on soil organic matter, and/or demethylation in drier wetland so

56 shaping surface litter contribution to soil organic matter as it responds to climate warming effects

57 rded in the presence of methanol and natural organic matter as sulfate radical scavengers.

58 s an important role in transforming effluent organic matter as wastewater effluents travel downstream

59 asured carbon isotopes in both carbonate and organic matter as well as their trace element compositio

60 iniferal metabolism compared to predation or organic matter assimilation is unknown.

61 lta(15) N was significantly enriched in soil organic matter at all depths than in the living plant ti

62 Fluorescent natural organic matter at tryptophan-like (TLF) and humic-like f

63 As climate warms, permafrost thaws and soil organic matter becomes vulnerable to greater microbial d

64 basic ecosystem functions (decomposition of organic matter, benthic primary production) by acting in

65 ibly within anaerobic microzones of settling organic matter, but MeHg (CH(3)Hg(+)) and Me(2)Hg ((CH(3

66 how a functional trait-the decomposition of organic matter, can be addressed based on genetic marker

67 oils globally(1), so destabilization of soil organic matter caused by the warming predicted for tropi

68 n quantum yields from chromophoric dissolved organic matter (CDOM) have been reported for many sample

69 tion of solar radiation by colored dissolved organic matter (CDOM) in surface waters results in the f

70 The photobleaching of chromophoric dissolved organic matter (CDOM) is considered an important loss pr

71 ariation in soil properties (pH, texture and organic matter), climatic conditions (Atlantic, alpine,

72 ctance, and a wastewater-derived fluorescent organic matter component) as the best combination of pre

73 lubility of CuO NP correlated well with soil organic matter content ( R(2) = 0.89) independent of soi

74 Our study suggests that soil pH and organic matter content affect the dissolution behavior o

75 While organic matter content and quality were commonly reporte

76 A change in soil organic matter content from 5.6% to 67.4% led to a 4.2-f

77 Fe(2+) release was strongly dependent on the organic matter content of the sediment.

78 mendments mitigated soil salinity, increased organic matter content, available water, hydraulic condu

79 this research were to quantify the impact of organic matter content, soil pH and moisture content on

80 pH < 6.3 ( R(2) = 0.89), independent of soil organic matter content.

81 h fungi potentially hold important roles for organic matter cycling and food web dynamics.

82 ents at Pendleton, OR (USA), were focused on organic matter cycling, but the consequences of land man

83 oth chemodiversity and genes associated with organic matter decomposition increased as more plant lit

84 First-order organic matter decomposition models are used within most

85 amental role on key ecosystem functions like organic matter decomposition, although how local assembl

86 this warming is projected to stimulate soil organic matter decomposition, and promote a positive fee

87 arming is projected to reduce by stimulating organic matter decomposition, creating a positive feedba

88 crobial processes that drive litter and soil organic matter decomposition.

89 ss, which may trade-off with traits enabling organic matter decomposition.

90 osition while genes involved in oxidation of organic matter decreased.

91 Fungal decomposition of soil organic matter depends on soil nitrogen (N) availability

92 to quantify how changes in the diversity of organic matter derived from plants (i.e. litter) affect

93 Oxidative decomposition of soil organic matter determines the proportion of carbon that

94 it carbon of the petroleum-derived dissolved organic matter (DOM(HC)) produced via photo-oxidation, h

95 reasingly employed to characterize dissolved organic matter (DOM) across a range of aquatic environme

96 vs. decomposition by adding (13)C dissolved organic matter (DOM) and (57)Fe(II) to soil slurries inc

97 een the optical properties of soil dissolved organic matter (DOM) and acidic functions carried out by

98 Both oxidants react with dissolved organic matter (DOM) and alter its composition, but the

99 opollutant degradation by the AOP, dissolved organic matter (DOM) and the disinfection byproduct (DBP

100 e impact of chlorine photolysis on dissolved organic matter (DOM) composition and DBP formation is in

101 tively altering the composition of dissolved organic matter (DOM) exported to the ocean.

102 Dissolved organic matter (DOM) has been shown to inhibit the oxida

103 Biogeochemical processing of dissolved organic matter (DOM) in headwater rivers regulates aquat

104 developing small-scale patterns of dissolved organic matter (DOM) in soil solutions of a soil column

105 erizing low molecular weight (LMW) dissolved organic matter (DOM) in soils and evaluating the availab

106 s and sunlight convert terrigenous dissolved organic matter (DOM) in surface waters to greenhouse gas

107 ly used in the characterization of dissolved organic matter (DOM) in the aquatic continuum.

108 chemical data, but we surmise that dissolved organic matter (DOM) influences mercury retention in wet

109 Photochemical reactions convert dissolved organic matter (DOM) into inorganic and low-molecular-we

110 Dissolved organic matter (DOM) is a natural photosensitizer that c

111 three-dimensional configuration of dissolved organic matter (DOM) is an important factor in determini

112 This dissolved organic matter (DOM) is sourced from readily leachable o

113 Dissolved organic matter (DOM) is ubiquitous in raw drinking water

114 impacted waters, but its impact on dissolved organic matter (DOM) is unknown.

115 ields (Phi(Delta)) of a variety of dissolved organic matter (DOM) isolates and natural waters.

116 Dissolved organic matter (DOM) plays a significant role in the tra

117 Our results show that dissolved organic matter (DOM) reduces toxic responses and modulat

118 structure of many compounds in the dissolved organic matter (DOM) remains largely unknown, the high s

119 Dissolved organic matter (DOM) represents a key component of carbo

120 ms of phosphorus incorporated into dissolved organic matter (DOM) that microbes with the necessary tr

121 lent mercury (Hg(II)) complexed in dissolved organic matter (DOM) to fish.

122 The composition of dissolved organic matter (DOM), as revealed by ultra-high-resoluti

123 ire on quantity and composition of dissolved organic matter (DOM), stream water nutrient concentratio

124 e typical molecular fingerprint of dissolved organic matter (DOM).

125 Streams and rivers metabolize dissolved organic matter (DOM).

126 al and photophysical properties of dissolved organic matter (DOM).

127 hnique for the characterization of dissolved organic matter (DOM).

128 ical transformation is affected by dissolved organic matter (DOM).

129 med nucleophilic moieties in model dissolved organic matter (DOM; Fluka humic acid) can react via the

130 e atmospheric CO(2) and sequester it as soil organic matter during natural succession.

131 ts of tryptophan yield excited triplet-state organic matters during sunlight irradiation and play an

132 ng-lasting impacts on nutrient cycling, soil organic matter dynamics and ecosystem functioning.

133 ictive framework for linking litter quality, organic matter dynamics and nutrient acquisition in fore

134 nlight, surface solar heating, and dissolved organic matter dynamics.

135 t experienced rapid heating, consistent with organic matter ejected during the formation of the crate

136 Saltwater intrusion and organic matter enrichment may increase sulphate reductio

137 ble to intermittent saltwater inundation and organic matter enrichment.

138 ucing conditions in peatlands and other high-organic matter environments.

139 lipids cutin and cutan, to yield extractable organic matter (EOM).

140 ion including the depletion of nutrients and organic matter, erosion and compaction.

141 n these elements and the source of dissolved organic matter, especially for I (JFJ and PDM) and Se (J

142 ly efficient at retaining and redistributing organic matter even as opportunistic and highly competit

143 alysis showed that the fluorescent dissolved organic matter (FDOM) composition produced from the heav

144 al increases in N and P supply will increase organic matter flows to metazoan food webs in detritus-b

145 on and anammox were likely linked to sinking organic matter fluxes and in situ primary productivity u

146 hat they receive little terrestrial input of organic matter for decomposition and CO(2) production, a

147 Arctic lagoons were probably related to high organic matter found in Arctic wastewater due to lower c

148 anes are formed upon chlorination of natural organic matter found in many drinking water sources.

149 5) N was recovered in the mineral-associated organic matter fraction through microbial anabolism, sug

150 perimental scenarios that increased sediment organic matter from 5 to 25% or darkened overlying water

151 To do this, we extracted organic matter from 7 plant species using solvents that

152 d S in near-neutral pH environments can turn organic matter from an As sink into a source.

153 s are central in the production of dissolved organic matter from fossil fuels.

154 ution of photochemically generated dissolved organic matter from oil spills.

155 olecular-level characterization of dissolved organic matter from the Amazon River and tributaries dur

156 tio (delta(15)N) of foraminifera shell-bound organic matter from three sediment cores was high, indic

157 ough our understanding of the nature of soil organic matter has recently been substantially revised,

158 e also positively correlated, with dissolved organic matter having stronger effects on microbes than

159 ted values (e.g., for Suwannee River Natural Organic Matter IHSS isolate: 1.8% vs 0.23-2.89%).

160 imilates CO(2) for the primary production of organic matter in all plants and algae, as well as in so

161 ructures tackling the current performance of organic matter in cutting edge technological sectors, su

162 The presence of organic matter in lacustrine mudstone sediments at Gale

163 hts into interactions of bacteria and labile organic matter in marine environments.

164 ormation, transformation, and utilization of organic matter in oil shale source rocks.

165 cted to increase as massive stocks of frozen organic matter in permafrost are liberated in a warming

166 ssolved oxygen in surface water, and greater organic matter in sediments during both seasons, suggest

167 otope signatures and radiocarbon activity of organic matter in soil profiles, we quantified the magni

168 tter (DOM) is sourced from readily leachable organic matter in surface soils and deeper centuries-to

169 he downward flux of high-density particulate organic matter in the form of salp faecal pellets.

170 nities that colonize and degrade particulate organic matter in the ocean [2-4].

171 ather by restrictions on microbial access to organic matter in the spatially heterogeneous soil envir

172 e mainly driven by the amount of sedimentary organic matter in the system as well as by seasonal vari

173 de rapidly dissolved likely associating with organic matter in the water column, transported to terre

174 ta(15)N) of intra-crystalline coral skeletal organic matter in three coral cores collected at this si

175 on the recently reported molecular weight of organic matter in urban aerosols (MW(OM)) and activity c

176 r composition of petroleum-derived dissolved organic matter, including abundant hydrocarbons and S-co

177 l functional genes involved in hydrolysis of organic matter increased with ambient N deposition while

178 icrobial processing of aggregate-unprotected organic matter inputs is key for soil fertility, long-te

179 nthropogenic alterations of the nutrient and organic matter inputs to surface waters.

180 bon cycling: Probabilistic Representation of Organic Matter Interactions within the Soil Environment

181 from the deconstruction of complex forms of organic matter into a wealth of smaller metabolic interm

182 nisms are central to the conversion of plant organic matter into SOC, yet the relationship between pl

183 The organic matter is depleted in (15)N relative to the terr

184 noic acids indicate that ~40% of sedimentary organic matter is of terrestrial origin.

185 Organic matter is preserved in the form of amorphous car

186 h regulates the distribution of fresh, algal organic matter, is the main control of bacterial communi

187 in the amended FSi + Cl fractions, the added organic matter led to negligible changes in percent ferr

188 id (SRFA) as a representative of the natural organic matter likely to associate with Fe(III).

189 entration suggests potential contribution of organic matter management to unlocking unavailable forms

190 of sulfate, nitrate, ammonium, black carbon, organic matter, mineral dust, and sea-salt over 2000-201

191 summer, possibly due to accelerated rates of organic matter mineralization or iron reduction beneath

192 hat anaerobic respiration, sparked by labile organic matter, mobilizes P in this seemingly well-drain

193 Bloom-derived organic matter, much of it occurring as polysaccharides,

194 BP) or-more generally-for the production of organic matter (net primary production, NPP).

195 rrent study was to identify soil conditions (organic matter, nitrogen, and moisture content) that alt

196 s work, we investigate the impact of natural organic matter (NOM) and light on silver nanoparticle (A

197 nds and other wetlands with abundant natural organic matter (NOM) are important sinks for antimony (S

198 ed the functional group chemistry of natural organic matter (NOM) associated with both U(IV) and U(VI

199 raquinone-2,6-disulfonate (AQDS) and natural organic matter (NOM) can act as electron shuttles thus f

200 Natural organic matter (NOM) can contribute to arsenic (As) mobi

201 change (IEX) can successfully remove natural organic matter (NOM) from surface water.

202 Natural organic matter (NOM) is a highly complex mixture of natu

203 Natural organic matter (NOM) is an important redox-active compon

204 Natural organic matter (NOM) is known to affect the microbial re

205 ransfer via redox-active particulate natural organic matter (NOM) is still unclear, especially consid

206 Natural organic matter (NOM) is the product of microbial and abi

207 e sinks for antimony (Sb), and solid natural organic matter (NOM) may play an important role in contr

208 We investigated the influence of natural organic matter (NOM) on the behavior of Pu(V) in the vad

209 In contrast, the addition of natural organic matter (NOM) significantly enhanced the yields o

210 es of complex mixtures (like oil and natural organic matter (NOM)) and increasing the number of the m

211 S(2) was retarded in the presence of natural organic matter (NOM), including Suwannee River natural o

212 ses such as corrosion, adsorption of natural organic matter (NOM), presence of capping agents, and ex

213 ciation of Hg(II) in the presence of natural organic matter (NOM; Suwannee River DOM) and 15 LMM thio

214 ificant biogeochemical changes, and cascaded organic matter, nutrients, Hg and other organically-boun

215 ts, (3) coprophilous spores, (4) sedimentary organic matter (OC and sedaDNA), (5) stable isotopes of

216 errors when changes in bulk density or soil organic matter occur.

217 the polymer was present within the dissolved organic matter of snow.

218 Organic matter (OM) amendment and plant colonization are

219 te addition impacts the preservation of soil organic matter (OM) are poorly understood.

220 There is growing belief that natural organic matter (OM) binds U(IV) and mediates its fate in

221 Knowledge on organic matter (OM) concentration and composition is of

222 community structure result in variations in organic matter (OM) degradation is not well understood.

223 ICR-MS) was developed to extract and analyze organic matter (OM) from microliter volumes of salt cont

224 Organic matter (OM) is the most important controlling fa

225 The global carbon cycle connects organic matter (OM) pools in soil, freshwater, and marin

226 highly reactive, environmentally ubiquitous organic matter (OM) sorbents that act as mediators of te

227 ains a large (1700 Pg C) terrestrial pool of organic matter (OM) that is susceptible to degradation a

228 nd release pulses of dissolved nutrients and organic matter (OM).

229 ectory of which may be greatly influenced by organic matter (OM).

230 he influence of chloride (Cl(-)) and natural organic matter on Cu speciation and associated redox tra

231 irectly detect the molecular partitioning of organic matter onto an iron oxyhydroxide during adsorpti

232 r DIC and shallow carbonate, without burying organic matter or generating O(2).

233 by autotrophic carbon cycling in addition to organic matter oxidation and anammox.

234 nd our understanding of specific pathways of organic matter oxidation by the heterotrophic SUP05.

235 cultivated in soils with different levels of organic matter (p < 0.001).

236 Dissolved organic matter plays an important role in aquatic ecosys

237 into and taken up from the marine dissolved organic matter pool by microorganisms, and the ecologica

238 land and govern the turnover of the largest organic matter pool in the terrestrial biosphere.

239 ibute this increased uptake to absorption by organic matter present in the indoor particles.

240 Characterizing organic matter preserved in archaeological sediment is c

241 e interception, processing, and retention of organic matter, prior to its export to the coastal ocean

242 eccias found to date and contains primordial organic matter, probably originating in the interstellar

243 such as nutrient uptake and transformation, organic matter processing, and ecosystem metabolism.

244 wastewater (WW) on microbial communities and organic-matter processing using a standardized decomposi

245 Organic matter production and decomposition primarily mo

246 ts suggest arsenic-based metabolisms support organic matter production and impact nitrogen biogeochem

247 In other words, in-lake organic matter production depends only on APS if the lat

248 (RubisCO), is a main determinant of de novo organic matter production on Earth.

249 s of the global ocean with elevated rates of organic matter production supporting major fisheries.

250 , while the marine P cycle would also affect organic matter production.

251 rge scale observations of heme b relative to organic matter provide further evidence of the impact of

252 Moreover, although organic matter released from OlV1- and OlV7-infected hos

253 biofilm reactors (MBBRs), achieving soluble organic matter removal, over a 64 day exposure to nomina

254 nputs have led to positive 'priming' of soil organic matter, resulting in SOC loss, constraining the

255 nds region of Alberta, Canada, and dissolved organic matter samples from the Suwannee River Fulvic Ac

256 particles (e.g., fine and coarse particulate organic matter) showed that particle diameter was positi

257 to access organic nitrogen (N) bound in soil organic matter (SOM) and transfer this growth-limiting n

258 The accumulation and decomposition of soil organic matter (SOM) are closely tied to mangroves' carb

259 rized by ferrihydrite (48%) and Fe(III)-soil organic matter (SOM) complexes (37%), whereas in the FSa

260 ionic PFAS correlated strongly with the soil organic matter (SOM) content and was reversible in all s

261 Soil organic matter (SOM) is an indicator of sustainable land

262 Soil organic matter (SOM) is correlated with reactive iron (F

263 Understanding the composition of soil organic matter (SOM) is vital to our understanding of ho

264 on of degraded alpine grassland on: (a) soil organic matter (SOM) mineralization; and (b) the importa

265 Managing soil organic matter (SOM) stocks to address global change cha

266 by thermally altering the chemistry of soil organic matter (SOM), thereby reducing rates of microbia

267 on, Utah, USA reveals dense accumulations of organic-matter spheres (30-50 mum diameter) of probable

268 tter (NOM), including Suwannee River natural organic matter (SRNOM) and Aldrich humic acid (ALHA), in

269 Moreover, Suwanee River Natural Organic Matter (SRNOM) has been used to analyze the effe

270 oot exudation, microbial processes, and soil organic matter stabilization.

271 ation of the hydrophobic layer and pyrolysed organic matter, such as hydrophobic surface binding prot

272 ion of the highest levels of enrichment with organic matter suggests either redox control or stabiliz

273 ts enhancing productivity and pH, as well as organic matter supporting excess respiration driving aci

274 presence of the chosen surrogate of natural organic matter, Suwannee river fulvic acid (SRFA).

275 plankton transform inorganic substrates into organic matter that fuels the activity of heterotrophic

276 the nitrogen-to-phosphorus ratio of exported organic matter that greatly increases the global nitroge

277 erm dynamics of vegetation, and thereby soil organic matter, that occur in response to thermal, hydro

278 types, a triglyceride mixture and dissolved organic matter, this method is compared to traditional e

279 With enrichment of organic matter, this system flips within three days from

280 ) potentially increases export of refractory organic matter through increased production of hydrolyti

281 the accumulation and mobility of plastic and organic matter through the column (analogous to a soil).

282 Full conversion of organic matter to CO(2) requires oxidative mechanisms th

283 s and macrophytes is a substantial source of organic matter to estuaries and therefore has the potent

284 dless of the amendment type, the addition of organic matter to soil increased the capability of the c

285 ltered SOM may allow a greater proportion of organic matter to survive vertical migration into satura

286 e plant growth, vegetation biomass, and soil organic matter; transferring carbon from the atmosphere

287 threaten essential ecosystem functions like organic matter turnover and nutrient cycling in future e

288 tems as hydrological inputs of nutrients and organic matter vary.

289 HZ, where removal of biodegradable dissolved organic matter was also the highest.

290 s spectrometry elucidated that any remaining organic matter was comprised of smaller and highly aliph

291 quantity and chemistry of water-extractable organic matter (WEOM) in the bulk soil and its heavy den

292 h nucleophilic adducts and bound residues in organic matter will facilitate transport and help mask d

293 from indoor sources, typically dominated by organic matter, will undergo such processes as well.

294 ing to an attenuation in the sinking flux of organic matter with depth.

295 The efficiency in decomposing organic matter with diluted acid was higher than 89%.

296 proximity between microbial decomposers and organic matter, with emphasis on their physical location

297 previously proposed layered accumulation of organic matter within aggregate organo-mineral microstru

298 We report on the detection of primordial organic matter within the carbonaceous chondrite Maribo

299 l and day-night variability of water-soluble organic matter (WSOM) composition.

300 Nonmethanesulfonic acid Water-Soluble Organic Matter (WSOM) represented 6-8% and 11-22% of the