Forest nitrogen sinks in large eastern U.S. watersheds: Estimates from forest inventory and an ecosystem model

Christine L. Goodale, Kate Lajtha, Knute J. Nadelhoffer, Elizabeth Weeks Boyer, Norbert A. Jaworski

Research output: Contribution to journalArticle

46 Citations (Scopus)

Abstract

The eastern U.S. receives elevated rates of N deposition compared to preindustrial times, yet relatively little of this N is exported in drainage waters. Net uptake of N into forest biomass and soils could account for a substantial portion of the difference between N deposition and solution exports. We quantified forest N sinks in biomass accumulation and harvest export for 16 large river basins in the eastern U.S. with two separate approaches: (1) using growth data from the USDA Forest Service's Forest Inventory and Analysis (FIA) program, and (2) using a model of forest nitrogen cycling (PnET-CN) linked to FIA information on forest age-class structure. The model was also used to quantify N sinks in soil and dead wood, and nitrate losses below the rooting zone. Both methods agreed that net growth rates were highest in the relatively young forests on the Schuylkill watershed, and lowest in the cool forests of northern Maine. Across the 16 watersheds, wood export removed an average of 2.7 kg N ha-1 yr-1 (range: 1-5 kg N ha-1 yr-1), and standing stocks increased by 4.0 kg N ha-1 yr-1 (-3 to 8 kg N ha-1 yr-1). Together, these sinks for N in woody biomass amounted to a mean of 6.7 kg N ha-1 yr-1 (2-9 kg N ha-1 yr-1), or 73% (15-115%) of atmospheric N deposition. Modeled rates of net N sinks in dead wood and soil were small; soils were only a significant net sink for N during simulations of reforestation of degraded agricultural sites. Predicted losses of nitrate depended on the combined effects of N deposition, and both short- and long-term effects of disturbance. Linking the model with forest inventory information on age-class structure provided a useful step toward incorporating realistic patterns of forest disturbance status across the landscape.

Original languageEnglish (US)
Pages (from-to)239-266
Number of pages28
JournalBiogeochemistry
Volume57-58
DOIs
StatePublished - Jul 27 2002

Fingerprint

forest inventory
Watersheds
Ecosystems
Nitrogen
watershed
Soils
Wood
Biomass
ecosystem
nitrogen
Nitrates
Reforestation
Information analysis
dead wood
biomass
age class
Catchments
Drainage
soil
Rivers

All Science Journal Classification (ASJC) codes

  • Environmental Chemistry
  • Water Science and Technology
  • Earth-Surface Processes

Cite this

Goodale, Christine L. ; Lajtha, Kate ; Nadelhoffer, Knute J. ; Boyer, Elizabeth Weeks ; Jaworski, Norbert A. / Forest nitrogen sinks in large eastern U.S. watersheds : Estimates from forest inventory and an ecosystem model. In: Biogeochemistry. 2002 ; Vol. 57-58. pp. 239-266.
@article{3e8ed52b82ce443b968eee5b3c2d1670,
title = "Forest nitrogen sinks in large eastern U.S. watersheds: Estimates from forest inventory and an ecosystem model",
abstract = "The eastern U.S. receives elevated rates of N deposition compared to preindustrial times, yet relatively little of this N is exported in drainage waters. Net uptake of N into forest biomass and soils could account for a substantial portion of the difference between N deposition and solution exports. We quantified forest N sinks in biomass accumulation and harvest export for 16 large river basins in the eastern U.S. with two separate approaches: (1) using growth data from the USDA Forest Service's Forest Inventory and Analysis (FIA) program, and (2) using a model of forest nitrogen cycling (PnET-CN) linked to FIA information on forest age-class structure. The model was also used to quantify N sinks in soil and dead wood, and nitrate losses below the rooting zone. Both methods agreed that net growth rates were highest in the relatively young forests on the Schuylkill watershed, and lowest in the cool forests of northern Maine. Across the 16 watersheds, wood export removed an average of 2.7 kg N ha-1 yr-1 (range: 1-5 kg N ha-1 yr-1), and standing stocks increased by 4.0 kg N ha-1 yr-1 (-3 to 8 kg N ha-1 yr-1). Together, these sinks for N in woody biomass amounted to a mean of 6.7 kg N ha-1 yr-1 (2-9 kg N ha-1 yr-1), or 73{\%} (15-115{\%}) of atmospheric N deposition. Modeled rates of net N sinks in dead wood and soil were small; soils were only a significant net sink for N during simulations of reforestation of degraded agricultural sites. Predicted losses of nitrate depended on the combined effects of N deposition, and both short- and long-term effects of disturbance. Linking the model with forest inventory information on age-class structure provided a useful step toward incorporating realistic patterns of forest disturbance status across the landscape.",
author = "Goodale, {Christine L.} and Kate Lajtha and Nadelhoffer, {Knute J.} and Boyer, {Elizabeth Weeks} and Jaworski, {Norbert A.}",
year = "2002",
month = "7",
day = "27",
doi = "10.1023/A:1015796616532",
language = "English (US)",
volume = "57-58",
pages = "239--266",
journal = "Biogeochemistry",
issn = "0168-2563",
publisher = "Springer Netherlands",

}

Forest nitrogen sinks in large eastern U.S. watersheds : Estimates from forest inventory and an ecosystem model. / Goodale, Christine L.; Lajtha, Kate; Nadelhoffer, Knute J.; Boyer, Elizabeth Weeks; Jaworski, Norbert A.

In: Biogeochemistry, Vol. 57-58, 27.07.2002, p. 239-266.

Research output: Contribution to journalArticle

TY - JOUR

T1 - Forest nitrogen sinks in large eastern U.S. watersheds

T2 - Estimates from forest inventory and an ecosystem model

AU - Goodale, Christine L.

AU - Lajtha, Kate

AU - Nadelhoffer, Knute J.

AU - Boyer, Elizabeth Weeks

AU - Jaworski, Norbert A.

PY - 2002/7/27

Y1 - 2002/7/27

N2 - The eastern U.S. receives elevated rates of N deposition compared to preindustrial times, yet relatively little of this N is exported in drainage waters. Net uptake of N into forest biomass and soils could account for a substantial portion of the difference between N deposition and solution exports. We quantified forest N sinks in biomass accumulation and harvest export for 16 large river basins in the eastern U.S. with two separate approaches: (1) using growth data from the USDA Forest Service's Forest Inventory and Analysis (FIA) program, and (2) using a model of forest nitrogen cycling (PnET-CN) linked to FIA information on forest age-class structure. The model was also used to quantify N sinks in soil and dead wood, and nitrate losses below the rooting zone. Both methods agreed that net growth rates were highest in the relatively young forests on the Schuylkill watershed, and lowest in the cool forests of northern Maine. Across the 16 watersheds, wood export removed an average of 2.7 kg N ha-1 yr-1 (range: 1-5 kg N ha-1 yr-1), and standing stocks increased by 4.0 kg N ha-1 yr-1 (-3 to 8 kg N ha-1 yr-1). Together, these sinks for N in woody biomass amounted to a mean of 6.7 kg N ha-1 yr-1 (2-9 kg N ha-1 yr-1), or 73% (15-115%) of atmospheric N deposition. Modeled rates of net N sinks in dead wood and soil were small; soils were only a significant net sink for N during simulations of reforestation of degraded agricultural sites. Predicted losses of nitrate depended on the combined effects of N deposition, and both short- and long-term effects of disturbance. Linking the model with forest inventory information on age-class structure provided a useful step toward incorporating realistic patterns of forest disturbance status across the landscape.

AB - The eastern U.S. receives elevated rates of N deposition compared to preindustrial times, yet relatively little of this N is exported in drainage waters. Net uptake of N into forest biomass and soils could account for a substantial portion of the difference between N deposition and solution exports. We quantified forest N sinks in biomass accumulation and harvest export for 16 large river basins in the eastern U.S. with two separate approaches: (1) using growth data from the USDA Forest Service's Forest Inventory and Analysis (FIA) program, and (2) using a model of forest nitrogen cycling (PnET-CN) linked to FIA information on forest age-class structure. The model was also used to quantify N sinks in soil and dead wood, and nitrate losses below the rooting zone. Both methods agreed that net growth rates were highest in the relatively young forests on the Schuylkill watershed, and lowest in the cool forests of northern Maine. Across the 16 watersheds, wood export removed an average of 2.7 kg N ha-1 yr-1 (range: 1-5 kg N ha-1 yr-1), and standing stocks increased by 4.0 kg N ha-1 yr-1 (-3 to 8 kg N ha-1 yr-1). Together, these sinks for N in woody biomass amounted to a mean of 6.7 kg N ha-1 yr-1 (2-9 kg N ha-1 yr-1), or 73% (15-115%) of atmospheric N deposition. Modeled rates of net N sinks in dead wood and soil were small; soils were only a significant net sink for N during simulations of reforestation of degraded agricultural sites. Predicted losses of nitrate depended on the combined effects of N deposition, and both short- and long-term effects of disturbance. Linking the model with forest inventory information on age-class structure provided a useful step toward incorporating realistic patterns of forest disturbance status across the landscape.

UR - http://www.scopus.com/inward/record.url?scp=18544397194&partnerID=8YFLogxK

UR - http://www.scopus.com/inward/citedby.url?scp=18544397194&partnerID=8YFLogxK

U2 - 10.1023/A:1015796616532

DO - 10.1023/A:1015796616532

M3 - Article

AN - SCOPUS:18544397194

VL - 57-58

SP - 239

EP - 266

JO - Biogeochemistry

JF - Biogeochemistry

SN - 0168-2563

ER -