Precipitation is the key determinant of topsoil δ15N values in southern Patagonia’s semiarid rangelands

Nitrogen (N) cycling in rangeland soils could potentially be controlled by water supply, stocking rates, or a range of other variables, such as ecosystem N stocks. To gauge the relative importance and elucidate possible interactions among these factors, we measured many abiotic variables to identif...

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Main Authors: Peri, Pablo Luis, Duarte Guardia, Sandra, Amelung, Wulf, Ladd, Brenton
Format: Artículo
Language:Inglés
Published: American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America 2022
Subjects:
Online Access:http://hdl.handle.net/20.500.12123/11351
https://acsess.onlinelibrary.wiley.com/doi/full/10.1002/vzj2.20183
https://doi.org/10.1002/vzj2.20183
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author Peri, Pablo Luis
Duarte Guardia, Sandra
Amelung, Wulf
Ladd, Brenton
author_browse Amelung, Wulf
Duarte Guardia, Sandra
Ladd, Brenton
Peri, Pablo Luis
author_facet Peri, Pablo Luis
Duarte Guardia, Sandra
Amelung, Wulf
Ladd, Brenton
author_sort Peri, Pablo Luis
collection INTA Digital
description Nitrogen (N) cycling in rangeland soils could potentially be controlled by water supply, stocking rates, or a range of other variables, such as ecosystem N stocks. To gauge the relative importance and elucidate possible interactions among these factors, we measured many abiotic variables to identify first-order controls of δ15N for Patagonia’s rangeland soils under contrasting historical grazing intensities. The results showed that δ15N values declined as water availability increased. The effects of precipitation and stocking rate on soil δ15N values were additive, and the effect of precipitation far outweighed the effects of grazing pressure. The soil N stock was a weak predictive variable for modeling variation in δ15N of the soil. Earlier assumptions about an inflection point for N cycling and δ15N values related to aridity were not confirmed. We conclude that variation in water availability drives variation in δ15N values irrespective of grazing intensity. We also conclude that meaningful interpretation of δ15N in soil will require a better mechanistic understanding of the interactions between water and N in the vadose zone than we currently possess.
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institution Instituto Nacional de Tecnología Agropecuaria (INTA -Argentina)
language Inglés
publishDate 2022
publishDateRange 2022
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publisher American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America
publisherStr American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America
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spelling INTA113512022-03-09T13:44:39Z Precipitation is the key determinant of topsoil δ15N values in southern Patagonia’s semiarid rangelands Peri, Pablo Luis Duarte Guardia, Sandra Amelung, Wulf Ladd, Brenton Nitrogen Precipitation Soil Rangelands Semiarid Zones Abiotic Factors Water Availability Grazing Intensity Interactions Shrubs Nitrógeno Precipitación Atmosférica Suelo Tierras de Pastos Zona Semiárida Factores Abióticos Disponibilidad del Agua Intensidad de Pastoreo Interacciones Santa Cruz (Argentina) Arbustos PEBANPA Network Tussock Short grasses Red PEBANPA Región Patagónica Pasto Pastos Cortos Nitrogen (N) cycling in rangeland soils could potentially be controlled by water supply, stocking rates, or a range of other variables, such as ecosystem N stocks. To gauge the relative importance and elucidate possible interactions among these factors, we measured many abiotic variables to identify first-order controls of δ15N for Patagonia’s rangeland soils under contrasting historical grazing intensities. The results showed that δ15N values declined as water availability increased. The effects of precipitation and stocking rate on soil δ15N values were additive, and the effect of precipitation far outweighed the effects of grazing pressure. The soil N stock was a weak predictive variable for modeling variation in δ15N of the soil. Earlier assumptions about an inflection point for N cycling and δ15N values related to aridity were not confirmed. We conclude that variation in water availability drives variation in δ15N values irrespective of grazing intensity. We also conclude that meaningful interpretation of δ15N in soil will require a better mechanistic understanding of the interactions between water and N in the vadose zone than we currently possess. EEA Santa Cruz Fil: Peri, Pablo Luis. Instituto Nacional de Tecnología Agropecuaria (INTA). Estación Experimental Agropecuaria Santa Cruz; Argentina. Fil: Peri, Pablo Luis. Universidad Nacional de la Patagonia Austral; Argentina. Fil: Peri, Pablo Luis. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Fil: Duarte Guardia, Sandra. Universidad Nacional de la Patagonia Austral; Argentina. Fil: Duarte Guardia, Sandra. Instituto Nacional de Innovación Agraria (INIA). Laboratorio Nacional de Suelos, Aguas y Foliares-LABSAF; Perú. Fil: Amelung, Wulf. University of Bonn. Institute of Crop Science and Resource Conservation (INRES). Soil Science and Soil Ecology; Alemania Fil: Ladd, Brenton. Universidad Científica del Sur. Escuela de Agroforestería; Perú. 2022-03-09T13:34:43Z 2022-03-09T13:34:43Z 2022-02-11 info:ar-repo/semantics/artículo info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion http://hdl.handle.net/20.500.12123/11351 https://acsess.onlinelibrary.wiley.com/doi/full/10.1002/vzj2.20183 Peri P.L.; Duarte-Guardia S.; Amelung W.; Ladd B. (2022) Precipitation is the key determinant of topsoil δ15N values in southern Patagonia’s semiarid rangelands. Vadose Zone Journal 21: e20183. DOI: 10.1002/vzj2.20183. 1539-1663 https://doi.org/10.1002/vzj2.20183 eng info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by-nc-sa/4.0/ Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-SA 4.0) application/pdf American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America Vadose Zone Journal 21: e20183. (First published: 11 February 2022)
spellingShingle Nitrogen
Precipitation
Soil
Rangelands
Semiarid Zones
Abiotic Factors
Water Availability
Grazing Intensity
Interactions
Shrubs
Nitrógeno
Precipitación Atmosférica
Suelo
Tierras de Pastos
Zona Semiárida
Factores Abióticos
Disponibilidad del Agua
Intensidad de Pastoreo
Interacciones
Santa Cruz (Argentina)
Arbustos
PEBANPA Network
Tussock
Short grasses
Red PEBANPA
Región Patagónica
Pasto
Pastos Cortos
Peri, Pablo Luis
Duarte Guardia, Sandra
Amelung, Wulf
Ladd, Brenton
Precipitation is the key determinant of topsoil δ15N values in southern Patagonia’s semiarid rangelands
title Precipitation is the key determinant of topsoil δ15N values in southern Patagonia’s semiarid rangelands
title_full Precipitation is the key determinant of topsoil δ15N values in southern Patagonia’s semiarid rangelands
title_fullStr Precipitation is the key determinant of topsoil δ15N values in southern Patagonia’s semiarid rangelands
title_full_unstemmed Precipitation is the key determinant of topsoil δ15N values in southern Patagonia’s semiarid rangelands
title_short Precipitation is the key determinant of topsoil δ15N values in southern Patagonia’s semiarid rangelands
title_sort precipitation is the key determinant of topsoil δ15n values in southern patagonia s semiarid rangelands
topic Nitrogen
Precipitation
Soil
Rangelands
Semiarid Zones
Abiotic Factors
Water Availability
Grazing Intensity
Interactions
Shrubs
Nitrógeno
Precipitación Atmosférica
Suelo
Tierras de Pastos
Zona Semiárida
Factores Abióticos
Disponibilidad del Agua
Intensidad de Pastoreo
Interacciones
Santa Cruz (Argentina)
Arbustos
PEBANPA Network
Tussock
Short grasses
Red PEBANPA
Región Patagónica
Pasto
Pastos Cortos
url http://hdl.handle.net/20.500.12123/11351
https://acsess.onlinelibrary.wiley.com/doi/full/10.1002/vzj2.20183
https://doi.org/10.1002/vzj2.20183
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AT laddbrenton precipitationisthekeydeterminantoftopsoild15nvaluesinsouthernpatagoniassemiaridrangelands