A seasonal nitrogen deposition budget for Rocky Mountain National Park

被引:58
|
作者
Benedict, K. B. [1 ]
Carrico, C. M. [1 ]
Kreidenweis, S. M. [1 ]
Schichtel, B. [2 ]
Malm, W. C. [2 ]
Collett, J. L., Jr. [1 ]
机构
[1] Colorado State Univ, Dept Atmospher Sci, Ft Collins, CO 80523 USA
[2] Colorado State Univ, Cooperat Inst Res Atmosphere, Natl Pk Serv, Ft Collins, CO 80523 USA
关键词
ammonia; atmospheric deposition; dry deposition; nitrogen; organic nitrogen; Rocky Mountains; wet deposition; SOLUBLE ORGANIC NITROGEN; COLORADO FRONT RANGE; CRITICAL LOADS; DRY DEPOSITION; ATMOSPHERIC DEPOSITION; REACTIVE NITROGEN; PRECIPITATION CHEMISTRY; ALPINE VEGETATION; MULTILAYER MODEL; WET DEPOSITION;
D O I
10.1890/12-1624.1
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
Nitrogen deposition is a concern in many protected ecosystems around the world, yet few studies have quantified a complete reactive nitrogen deposition budget including all dry and wet, inorganic and organic compounds. Critical loads that identify the level at which nitrogen deposition negatively affects an ecosystem are often defined using incomplete reactive nitrogen budgets. Frequently only wet deposition of ammonium and nitrate are considered, despite the importance of other nitrogen deposition pathways. Recently, dry deposition pathways including particulate ammonium and nitrate and gas phase nitric acid have been added to nitrogen deposition budgets. However, other nitrogen deposition pathways, including dry deposition of ammonia and wet deposition of organic nitrogen, still are rarely included. In this study, a more complete seasonal nitrogen deposition budget was constructed based on observations during a year-long study period from November 2008 to November 2009 at a location on the east side of Rocky Mountain National Park (RMNP), Colorado, USA. Measurements included wet deposition of ammonium, nitrate, and organic nitrogen, PM2.5 (particulate matter with an aerodynamic diameter less than 2.5 mu m, nitrate, and ammonium) concentrations of ammonium, nitrate, and organic nitrogen, and atmospheric gas phase concentrations of ammonia, nitric acid, and NO2. Dry deposition fluxes were determined from measured ambient concentrations and modeled deposition velocities. Total reactive nitrogen deposition by all included pathways was found to be 3.65 kg N center dot ha(-1)yr(-1). Monthly deposition fluxes ranged from 0.06 to 0.54 kg N center dot ha(-1)yr(-1), with peak deposition in the month of July and the least deposition in December. Wet deposition of ammonium and nitrate were the two largest deposition pathways, together contributing 1.97 kg N center dot ha(-1)yr(-1) or 54% of the total nitrogen deposition budget for this region. The next two largest deposition pathways were wet deposition of organic nitrogen and dry deposition of ammonia; combined they contributed 1.37 kg N center dot ha(-1)yr(-1) or 37% of the total nitrogen deposition budget. To better understand the nitrogen cycle and key interactions between the atmosphere and biosphere we need to include as many sources and types of nitrogen as possible and understand their variability throughout the year. Here we examine the components of the nitrogen deposition budget to better understand the factors that influence the different deposition pathways and their seasonal variations.
引用
收藏
页码:1156 / 1169
页数:14
相关论文
共 50 条
  • [21] Mercury transport in a high-elevation watershed in Rocky Mountain National Park, Colorado
    Mast, MA
    Campbell, DH
    Krabbenhoft, DP
    Taylor, HE
    WATER AIR AND SOIL POLLUTION, 2005, 164 (1-4): : 21 - 42
  • [22] Long-term ecosystem and biogeochemical research in Loch Vale watershed, Rocky Mountain National Park, Colorado
    Baron, Jill S.
    Clow, David W.
    Oleksy, Isabella A.
    Weinmann, Timothy
    Charlton, Caitlin
    Jayo, Amanda
    HYDROLOGICAL PROCESSES, 2021, 35 (03)
  • [23] Hydrologic restoration of a fen in Rocky Mountain National Park, Colorado, USA
    Cooper, DJ
    MacDonald, LH
    Wenger, SK
    Woods, SW
    WETLANDS, 1998, 18 (03) : 335 - 345
  • [24] Hydrologic restoration of a fen in Rocky Mountain National Park, Colorado, USA
    David J. Cooper
    Lee H. MacDonald
    Shaunda K. Wenger
    Scott W. Woods
    Wetlands, 1998, 18 : 335 - 345
  • [25] Nitrogen emission and deposition budget in West and Central Africa
    Galy-Lacaux, C.
    Delon, C.
    ENVIRONMENTAL RESEARCH LETTERS, 2014, 9 (12):
  • [26] Ammonia Emissions from Subalpine Forest and Mountain Grassland Soils in Rocky Mountain National Park
    Stratton, Joshua J.
    Ham, Jay
    Borch, Thomas
    JOURNAL OF ENVIRONMENTAL QUALITY, 2018, 47 (04) : 778 - 785
  • [27] Volatile organic compounds and ozone in Rocky Mountain National Park during FRAPPE
    Benedict, Katherine B.
    Zhou, Yong
    Sive, Barkley C.
    Prenni, Anthony J.
    Gebhart, Kristi A.
    Fischer, Emily V.
    Evanoski-Cole, Ashley
    Sullivan, Amy P.
    Callahan, Sara
    Schichtel, Bret A.
    Mao, Huiting
    Zhou, Ying
    Collett, Jeffrey L., Jr.
    ATMOSPHERIC CHEMISTRY AND PHYSICS, 2019, 19 (01) : 499 - 521
  • [28] Assessment of lake sensitivity to acidic deposition in national parks of the Rocky Mountains
    Nanus, L.
    Williams, M. W.
    Campbell, D. H.
    Tonnessen, K. A.
    Blett, T.
    Clow, D. W.
    ECOLOGICAL APPLICATIONS, 2009, 19 (04) : 961 - 973
  • [29] Back-trajectory-based source apportionment of airborne sulfur and nitrogen concentrations at Rocky Mountain National Park, Colorado, USA
    Gebhart, Kristi A.
    Schichtel, Bret A.
    Malm, William C.
    Barna, Michael G.
    Rodriguez, Marco A.
    Collett, Jeffrey L., Jr.
    ATMOSPHERIC ENVIRONMENT, 2011, 45 (03) : 621 - 633
  • [30] The atmospheric budget of oxidized nitrogen and its role in ozone formation and deposition
    Fowler, D
    Flechard, C
    Skiba, U
    Coyle, M
    Cape, JN
    NEW PHYTOLOGIST, 1998, 139 (01) : 11 - 23