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Ding Y, Shi Q, OuYang L, Lai B, Lai C, Yao G, Wang Z, Jia B. Isotopic source identification of nitrogen pollution in the Pi River in Chengdu. INTEGRATED ENVIRONMENTAL ASSESSMENT AND MANAGEMENT 2022; 18:1609-1620. [PMID: 35118803 DOI: 10.1002/ieam.4589] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 11/19/2021] [Revised: 01/31/2022] [Accepted: 02/01/2022] [Indexed: 06/14/2023]
Abstract
This study used stable isotope (δ15 N- NO 3 - and δ18 O- NO 3 - ) ratios, modeled by means of a Bayesian stable isotope analysis in R (SIAR) approach, to identify nitrate sources in the Pi River, which flows through the megacity Chengdu. The goal was to determine where management resources should be applied to reduce nitrogen pollution. Results revealed that NO 3 - was the primary nitrogen species throughout the study area; that it originated in manure and sewage, as well as nitrification of fertilizer and soil nitrogen; and that the nitrogen in the main stream came primarily from the tributaries. Notably, the nitrogen concentration in the tributaries exhibited no evident seasonal variations, further demonstrating that its source was intensive anthropogenic activity. Results of Bayesian model (SIAR) estimation indicated that manure and sewage were the dominant nitrate contributors in the watershed and that the nitrate concentration decreased from 54.19% to 39.57% in response to water treatment. These results empirically demonstrate that the methodology described in this work can be used effectively in catchments affected by intensive anthropogenic activity to determine where management resources should be applied to reduce nitrogen pollution. Integr Environ Assess Manag 2022;18:1609-1620. © 2022 SETAC.
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Affiliation(s)
- Yao Ding
- College of Architecture & Environment, Sichuan University, Chengdu, P.R. China
- Chengdu Institute of Environmental Protection, Chengdu, P.R. China
| | - Qing Shi
- Chengdu Institute of Environmental Protection, Chengdu, P.R. China
| | - Lili OuYang
- Chengdu Institute of Environmental Protection, Chengdu, P.R. China
| | - Bo Lai
- College of Architecture & Environment, Sichuan University, Chengdu, P.R. China
| | - Chengyue Lai
- Chengdu Institute of Environmental Protection, Chengdu, P.R. China
| | - Gang Yao
- College of Architecture & Environment, Sichuan University, Chengdu, P.R. China
- Institute for Environmental Engineering of RWTH Aachen University, Nordrhein-Westfalen, Germany
| | - Zhaoli Wang
- Chengdu Institute of Environmental Protection, Chengdu, P.R. China
| | - Binyang Jia
- Chengdu Operation Center for Environmental Emergencie, Chengdu, P.R. China
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2
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Buizert C, Fudge TJ, Roberts WHG, Steig EJ, Sherriff-Tadano S, Ritz C, Lefebvre E, Edwards J, Kawamura K, Oyabu I, Motoyama H, Kahle EC, Jones TR, Abe-Ouchi A, Obase T, Martin C, Corr H, Severinghaus JP, Beaudette R, Epifanio JA, Brook EJ, Martin K, Chappellaz J, Aoki S, Nakazawa T, Sowers TA, Alley RB, Ahn J, Sigl M, Severi M, Dunbar NW, Svensson A, Fegyveresi JM, He C, Liu Z, Zhu J, Otto-Bliesner BL, Lipenkov VY, Kageyama M, Schwander J. Antarctic surface temperature and elevation during the Last Glacial Maximum. Science 2021; 372:1097-1101. [PMID: 34083489 DOI: 10.1126/science.abd2897] [Citation(s) in RCA: 25] [Impact Index Per Article: 8.3] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 06/18/2020] [Accepted: 04/29/2021] [Indexed: 11/02/2022]
Abstract
Water-stable isotopes in polar ice cores are a widely used temperature proxy in paleoclimate reconstruction, yet calibration remains challenging in East Antarctica. Here, we reconstruct the magnitude and spatial pattern of Last Glacial Maximum surface cooling in Antarctica using borehole thermometry and firn properties in seven ice cores. West Antarctic sites cooled ~10°C relative to the preindustrial period. East Antarctic sites show a range from ~4° to ~7°C cooling, which is consistent with the results of global climate models when the effects of topographic changes indicated with ice core air-content data are included, but less than those indicated with the use of water-stable isotopes calibrated against modern spatial gradients. An altered Antarctic temperature inversion during the glacial reconciles our estimates with water-isotope observations.
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Affiliation(s)
- Christo Buizert
- College of Earth Ocean and Atmospheric Sciences, Oregon State University, Corvallis, OR 97331, USA.
| | - T J Fudge
- Department of Earth and Space Science, University of Washington, Seattle, WA 98195, USA
| | - William H G Roberts
- Geographical and Environmental Sciences, Northumbria University, Newcastle, UK
| | - Eric J Steig
- Department of Earth and Space Science, University of Washington, Seattle, WA 98195, USA
| | - Sam Sherriff-Tadano
- Atmosphere and Ocean Research Institute, The University of Tokyo, Kashiwa 277-8568, Japan
| | - Catherine Ritz
- Université Grenoble Alpes, CNRS, IRD, IGE, Grenoble, France
| | - Eric Lefebvre
- Université Grenoble Alpes, CNRS, IRD, IGE, Grenoble, France
| | - Jon Edwards
- College of Earth Ocean and Atmospheric Sciences, Oregon State University, Corvallis, OR 97331, USA
| | - Kenji Kawamura
- National Institute of Polar Research, Tachikawa, Tokyo, Japan.,Department of Polar Science, The Graduate University of Advanced Studies (SOKENDAI), Tokyo, Japan.,Japan Agency for Marine Science and Technology (JAMSTEC), Yokosuka, Japan
| | - Ikumi Oyabu
- National Institute of Polar Research, Tachikawa, Tokyo, Japan
| | | | - Emma C Kahle
- Department of Earth and Space Science, University of Washington, Seattle, WA 98195, USA
| | - Tyler R Jones
- Institute of Arctic and Alpine Research, University of Colorado, Boulder, CO 80309, USA
| | - Ayako Abe-Ouchi
- Atmosphere and Ocean Research Institute, The University of Tokyo, Kashiwa 277-8568, Japan
| | - Takashi Obase
- Atmosphere and Ocean Research Institute, The University of Tokyo, Kashiwa 277-8568, Japan
| | | | - Hugh Corr
- British Antarctic Survey, Cambridge, UK
| | - Jeffrey P Severinghaus
- Scripps Institution of Oceanography, University of California, San Diego, La Jolla, CA 92093, USA
| | - Ross Beaudette
- Scripps Institution of Oceanography, University of California, San Diego, La Jolla, CA 92093, USA
| | - Jenna A Epifanio
- College of Earth Ocean and Atmospheric Sciences, Oregon State University, Corvallis, OR 97331, USA
| | - Edward J Brook
- College of Earth Ocean and Atmospheric Sciences, Oregon State University, Corvallis, OR 97331, USA
| | - Kaden Martin
- College of Earth Ocean and Atmospheric Sciences, Oregon State University, Corvallis, OR 97331, USA
| | | | - Shuji Aoki
- Center for Atmospheric and Oceanic Studies, Graduate School of Science, Tohoku University, Sendai 980-8578, Japan
| | - Takakiyo Nakazawa
- Center for Atmospheric and Oceanic Studies, Graduate School of Science, Tohoku University, Sendai 980-8578, Japan
| | - Todd A Sowers
- School of Earth and Environmental Sciences, Seoul National University, Seoul 08826, South Korea
| | - Richard B Alley
- The Earth and Environmental Systems Institute, Pennsylvania State University, University Park, PA 16802, USA
| | - Jinho Ahn
- School of Earth and Environmental Sciences, Seoul National University, Seoul 08826, South Korea
| | - Michael Sigl
- Climate and Environmental Physics, Physics Institute & Oeschger Center for Climate Change Research, University of Bern, 3012 Bern, Switzerland
| | - Mirko Severi
- Department of Chemistry "Ugo Schiff," University of Florence, Florence, Italy.,Institute of Polar Sciences, ISP-CNR, Venice-Mestre, Italy
| | - Nelia W Dunbar
- New Mexico Bureau of Geology & Mineral Resources, Earth and Environmental Science Department, New Mexico Tech, Socorro, NM 87801, USA
| | - Anders Svensson
- Niels Bohr Institute, University of Copenhagen, Copenhagen, Denmark
| | - John M Fegyveresi
- School of Earth and Sustainability, Northern Arizona University, Flagstaff, AZ 86011, USA
| | - Chengfei He
- Department of Geography, Ohio State University, Columbus, OH 43210, USA
| | - Zhengyu Liu
- Department of Geography, Ohio State University, Columbus, OH 43210, USA
| | - Jiang Zhu
- National Center for Atmospheric Research, Boulder, CO 80307, USA
| | | | - Vladimir Y Lipenkov
- Climate and Environmental Research Laboratory, Arctic and Antarctic Research Institute, St. Petersburg 199397, Russia
| | - Masa Kageyama
- Laboratoire des Sciences du Climat et de l'Environnement-IPSL, Université Paris-Saclay, Gif-sur-Yvette, France
| | - Jakob Schwander
- Climate and Environmental Physics, Physics Institute & Oeschger Center for Climate Change Research, University of Bern, 3012 Bern, Switzerland
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Salamalikis V, Argiriou AA, Dotsika E. Isotopic modeling of the sub-cloud evaporation effect in precipitation. THE SCIENCE OF THE TOTAL ENVIRONMENT 2016; 544:1059-1072. [PMID: 26779956 DOI: 10.1016/j.scitotenv.2015.11.072] [Citation(s) in RCA: 5] [Impact Index Per Article: 0.6] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Subscribe] [Scholar Register] [Received: 09/17/2015] [Revised: 11/09/2015] [Accepted: 11/14/2015] [Indexed: 06/05/2023]
Abstract
In dry and warm environments sub-cloud evaporation influences the falling raindrops modifying their final stable isotopic content. During their descent from the cloud base towards the ground surface, through the unsaturated atmosphere, hydrometeors are subjected to evaporation whereas the kinetic fractionation results to less depleted or enriched isotopic signatures compared to the initial isotopic composition of the raindrops at cloud base. Nowadays the development of Generalized Climate Models (GCMs) that include isotopic content calculation modules are of great interest for the isotopic tracing of the global hydrological cycle. Therefore the accurate description of the underlying processes affecting stable isotopic content can improve the performance of iso-GCMs. The aim of this study is to model the sub-cloud evaporation effect using a) mixing and b) numerical isotope evaporation models. The isotope-mixing evaporation model simulates the isotopic enrichment (difference between the ground and the cloud base isotopic composition of raindrops) in terms of raindrop size, ambient temperature and relative humidity (RH) at ground level. The isotopic enrichment (Δδ) varies linearly with the evaporated raindrops mass fraction of the raindrop resulting to higher values at drier atmospheres and for smaller raindrops. The relationship between Δδ and RH is described by a 'heat capacity' model providing high correlation coefficients for both isotopes (R(2)>80%) indicating that RH is an ideal indicator of the sub-cloud evaporation effect. Vertical distribution of stable isotopes in falling raindrops is also investigated using a numerical isotope-evaporation model. Temperature and humidity dependence of the vertical isotopic variation is clearly described by the numerical isotopic model showing an increase in the isotopic values with increasing temperature and decreasing RH. At an almost saturated atmosphere (RH=95%) sub-cloud evaporation is negligible and the isotopic composition hardly changes even at high temperatures while at drier and warm conditions the enrichment of (18)Ο reaches up to 20‰, depending on the raindrop size and the initial meteorological conditions.
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Affiliation(s)
- V Salamalikis
- Laboratory of Atmospheric Physics, Department of Physics, University of Patras, GR 26500 Patras, Greece.
| | - A A Argiriou
- Laboratory of Atmospheric Physics, Department of Physics, University of Patras, GR 26500 Patras, Greece
| | - E Dotsika
- Stable Isotope Unit, Institute of Nanoscience and Nanotechnology, National Center of Scientific Research 'Demokritos', Ag. Paraskevi Attikis, 15310 Athens, Greece
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