Matches in SemOpenAlex for { <https://semopenalex.org/work/W2974366900> ?p ?o ?g. }
- W2974366900 endingPage "274" @default.
- W2974366900 startingPage "265" @default.
- W2974366900 abstract "Abstract. Understanding the production pathways of potent greenhouse gases, such as nitrous oxide (N2O), is essential for accurate flux prediction and for developing effective adaptation and mitigation strategies in response to climate change. Yet there remain surprising gaps in our understanding and precise quantification of the underlying production pathways – such as the relationship between soil moisture and N2O production pathways. A powerful, but arguably underutilized, approach for quantifying the relative contribution of nitrification and denitrification to N2O production involves determining 15N2O isotopomers and 15N site preference (SP) via spectroscopic techniques. Using one such technique, we conducted a short-term incubation where N2O production and 15N2O isotopomers were measured 24 h after soil moisture treatments of 40 % to 105 % water-filled pore space (WFPS) were established for each of three soils that differed in nutrient levels, organic matter, and texture. Relatively low N2O fluxes and high SP values indicted nitrification during dry soil conditions, whereas at higher soil moisture, peak N2O emissions coincided with a sharp decline in SP, indicating denitrification. This pattern supports the classic N2O production curves from nitrification and denitrification as inferred by earlier research; however, our isotopomer data enabled the quantification of source partitioning for either pathway. At soil moisture levels < 53 % WFPS, the fraction of N2O attributed to nitrification (FN) predominated but thereafter decreased rapidly with increasing soil moisture (x), according to FN=3.19-0.041x, until a WFPS of 78 % was reached. Simultaneously, from WFPS of 53 % to 78 %, the fraction of N2O that was attributed to denitrification (FD) was modelled as FD=-2.19+0.041x; at moisture levels of > 78 %, denitrification completely dominated. Clearly, the soil moisture level during transition is a key regulator of N2O production pathways. The presented equations may be helpful for other researchers in estimating N2O source partitioning when soil moisture falls within the transition from nitrification to denitrification." @default.
- W2974366900 created "2019-09-26" @default.
- W2974366900 creator A5027125669 @default.
- W2974366900 creator A5037465140 @default.
- W2974366900 creator A5038966837 @default.
- W2974366900 date "2019-09-19" @default.
- W2974366900 modified "2023-10-01" @default.
- W2974366900 title "A new look at an old concept: using <sup>15</sup>N<sub>2</sub>O isotopomers to understand the relationship between soil moisture and N<sub>2</sub>O production pathways" @default.
- W2974366900 cites W1562258491 @default.
- W2974366900 cites W1671606636 @default.
- W2974366900 cites W176811721 @default.
- W2974366900 cites W1877905106 @default.
- W2974366900 cites W1903052351 @default.
- W2974366900 cites W1983604861 @default.
- W2974366900 cites W2004002340 @default.
- W2974366900 cites W2024010831 @default.
- W2974366900 cites W2024385684 @default.
- W2974366900 cites W2028887543 @default.
- W2974366900 cites W2037893757 @default.
- W2974366900 cites W2049756681 @default.
- W2974366900 cites W2054654287 @default.
- W2974366900 cites W2056137498 @default.
- W2974366900 cites W2079506117 @default.
- W2974366900 cites W2086118270 @default.
- W2974366900 cites W2094455207 @default.
- W2974366900 cites W2100437772 @default.
- W2974366900 cites W2104982529 @default.
- W2974366900 cites W2112890395 @default.
- W2974366900 cites W2113177832 @default.
- W2974366900 cites W2117452501 @default.
- W2974366900 cites W2129469195 @default.
- W2974366900 cites W2133813560 @default.
- W2974366900 cites W2158085678 @default.
- W2974366900 cites W2158765373 @default.
- W2974366900 cites W2180779804 @default.
- W2974366900 cites W2216418590 @default.
- W2974366900 cites W2474948965 @default.
- W2974366900 cites W2485450699 @default.
- W2974366900 cites W2544613878 @default.
- W2974366900 cites W2558333456 @default.
- W2974366900 cites W2588110914 @default.
- W2974366900 cites W2592948058 @default.
- W2974366900 cites W4248585382 @default.
- W2974366900 doi "https://doi.org/10.5194/soil-5-265-2019" @default.
- W2974366900 hasPublicationYear "2019" @default.
- W2974366900 type Work @default.
- W2974366900 sameAs 2974366900 @default.
- W2974366900 citedByCount "33" @default.
- W2974366900 countsByYear W29743669002020 @default.
- W2974366900 countsByYear W29743669002021 @default.
- W2974366900 countsByYear W29743669002022 @default.
- W2974366900 countsByYear W29743669002023 @default.
- W2974366900 crossrefType "journal-article" @default.
- W2974366900 hasAuthorship W2974366900A5027125669 @default.
- W2974366900 hasAuthorship W2974366900A5037465140 @default.
- W2974366900 hasAuthorship W2974366900A5038966837 @default.
- W2974366900 hasBestOaLocation W29743669001 @default.
- W2974366900 hasConcept C107872376 @default.
- W2974366900 hasConcept C127413603 @default.
- W2974366900 hasConcept C159390177 @default.
- W2974366900 hasConcept C159750122 @default.
- W2974366900 hasConcept C164752452 @default.
- W2974366900 hasConcept C176864760 @default.
- W2974366900 hasConcept C178790620 @default.
- W2974366900 hasConcept C185592680 @default.
- W2974366900 hasConcept C187320778 @default.
- W2974366900 hasConcept C24939127 @default.
- W2974366900 hasConcept C2777573673 @default.
- W2974366900 hasConcept C2780138947 @default.
- W2974366900 hasConcept C39432304 @default.
- W2974366900 hasConcept C49045045 @default.
- W2974366900 hasConcept C537208039 @default.
- W2974366900 hasConcept C6557445 @default.
- W2974366900 hasConcept C73593433 @default.
- W2974366900 hasConcept C86803240 @default.
- W2974366900 hasConceptScore W2974366900C107872376 @default.
- W2974366900 hasConceptScore W2974366900C127413603 @default.
- W2974366900 hasConceptScore W2974366900C159390177 @default.
- W2974366900 hasConceptScore W2974366900C159750122 @default.
- W2974366900 hasConceptScore W2974366900C164752452 @default.
- W2974366900 hasConceptScore W2974366900C176864760 @default.
- W2974366900 hasConceptScore W2974366900C178790620 @default.
- W2974366900 hasConceptScore W2974366900C185592680 @default.
- W2974366900 hasConceptScore W2974366900C187320778 @default.
- W2974366900 hasConceptScore W2974366900C24939127 @default.
- W2974366900 hasConceptScore W2974366900C2777573673 @default.
- W2974366900 hasConceptScore W2974366900C2780138947 @default.
- W2974366900 hasConceptScore W2974366900C39432304 @default.
- W2974366900 hasConceptScore W2974366900C49045045 @default.
- W2974366900 hasConceptScore W2974366900C537208039 @default.
- W2974366900 hasConceptScore W2974366900C6557445 @default.
- W2974366900 hasConceptScore W2974366900C73593433 @default.
- W2974366900 hasConceptScore W2974366900C86803240 @default.
- W2974366900 hasFunder F4320334593 @default.
- W2974366900 hasIssue "2" @default.
- W2974366900 hasLocation W29743669001 @default.
- W2974366900 hasOpenAccess W2974366900 @default.
- W2974366900 hasPrimaryLocation W29743669001 @default.