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  • 1
    Online Resource
    Online Resource
    Canadian Science Publishing ; 2000
    In:  Canadian Journal of Forest Research Vol. 30, No. 9 ( 2000-09-01), p. 1476-1488
    In: Canadian Journal of Forest Research, Canadian Science Publishing, Vol. 30, No. 9 ( 2000-09-01), p. 1476-1488
    Abstract: Inorganic nitrogen (N) and sulfur (S) deposition in bulk throughfall and fog were determined at two sites located at opposite ends (42 km apart) of a pollution gradient in the San Bernardino Mountains. Plot-level averages for total annual N and S deposition in throughfall in 1996 were 18.8 and 2.9 kg·ha -1 , respectively, at Camp Paivika (CP) and 2.9 and 0.4 kg·ha -1 , respectively, at Barton Flats (BF). Deposition of N in throughfall in the four transects at CP ranged from 12.1 to 31.7 kg·ha -1 ·year -1 . Spatial variability was high because of heterogenous canopy cover and varying exposure to air pollution. Annual estimated stand-level deposition of N and S in fog were 10.9 and 1.9 kg·ha -1 , respectively, at CP, and 0.6 and 0.2 kg·ha -1 , respectively, at BF. We estimated that N deposition in fog contributed 35% of the total annual N deposition at CP and 13% at BF. Analogous values for S were 39% at CP and 26% at BF. Ammonium deposition in throughfall and fog at CP were 72 and 122% as high as NO 3 - deposition because of elevated NH 3 emissions from dairy farms in the Chino-Norco area 34 km southwest of CP.
    Type of Medium: Online Resource
    ISSN: 0045-5067 , 1208-6037
    Language: English
    Publisher: Canadian Science Publishing
    Publication Date: 2000
    detail.hit.zdb_id: 1473096-0
    SSG: 23
    SSG: 12
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  • 2
    Online Resource
    Online Resource
    Hindawi Limited ; 2001
    In:  The Scientific World JOURNAL Vol. 1 ( 2001), p. 433-439
    In: The Scientific World JOURNAL, Hindawi Limited, Vol. 1 ( 2001), p. 433-439
    Abstract: Virtually complete nitrification of the available ammonium in soil and nitrification activity in the forest floor are important factors predisposing forests in the San Bernardino Mountains of southern California to nitrogen (N) saturation. As a result, inorganic N in the soil solution is dominated by nitrate. High nitrification rates also generate elevated nitric oxide (NO) emissions from soil. High-base cation saturation of these soils means that soil calcium depletion or effects associated with soil acidification are not an immediate risk for forest health as has been postulated for mesic forests in the eastern U.S. Physiological disturbance (e.g., altered carbon [C] cycling, reduced fine root biomass, premature needle abscission) of ozone-sensitive ponderosa pine trees exposed to high N deposition and high ozone levels appear to be the greater threat to forest sustainability. However, N deposition appears to offset the aboveground growth depression effects of ozone exposure. High nitrification activity reported for many western ecosystems suggests that with chronic N inputs these systems are prone to N saturation and hydrologic and gaseous losses of N. High runoff during the winter wet season in California forests under a Mediterranean climate may further predispose these watersheds to high nitrate leachate losses. After 4 years of N fertilization at a severely N saturated site in the San Bernardino Mountains, bole growth unexpectedly increased. Reduced C allocation below- ground at this site, presumably in response to ozone or N or both pollutants, may enhance the bole growth response to added N.
    Type of Medium: Online Resource
    ISSN: 1537-744X
    Language: English
    Publisher: Hindawi Limited
    Publication Date: 2001
    detail.hit.zdb_id: 2075968-X
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  • 3
    Online Resource
    Online Resource
    Elsevier BV ; 2004
    In:  Forest Ecology and Management Vol. 200, No. 1-3 ( 2004-10), p. 67-76
    In: Forest Ecology and Management, Elsevier BV, Vol. 200, No. 1-3 ( 2004-10), p. 67-76
    Type of Medium: Online Resource
    ISSN: 0378-1127
    Language: English
    Publisher: Elsevier BV
    Publication Date: 2004
    detail.hit.zdb_id: 2016648-5
    detail.hit.zdb_id: 751138-3
    SSG: 23
    SSG: 12
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  • 4
    Online Resource
    Online Resource
    Canadian Science Publishing ; 1995
    In:  Canadian Journal of Forest Research Vol. 25, No. 1 ( 1995-01-01), p. 88-100
    In: Canadian Journal of Forest Research, Canadian Science Publishing, Vol. 25, No. 1 ( 1995-01-01), p. 88-100
    Abstract: Throughfall chemistry was studied in ponderosa pine (Pinusponderosa Laws.) seedlings exposed to wet and dry acidic deposition, ozone (O 3 ), drought, and nitric acid (HNO 3 ) in open-top chambers in the Sierra Nevada of California from 1988 to 1990. Seven acid rain events (pH 3.5, 4.4, and 5.3) occurred during each growing season. Acidity of the simulated rain treatments had little effect on net throughfall fluxes except for greater net SO 4 2− content in throughfall of the pH 3.5 treatment. Electrical conductivity and NO 3 − and NH 4 + content of throughfall were significantly higher in the NF150 treatment (1.5 × ambient O 3 ) than in the charcoal-filtered (CF) or non-charcoal-filtered (NF) treatments in all 3 years. Throughfall acidity in the NF150 treatment was higher than that in the CF or NF treatment during the last 2 years of the study. Effects of the NF150 treatment on throughfall chemistry were attributed primarily to deposition of HNO 3 from higher N oxides produced by the air-supplied O 3 generator. The concentration of HNO 3 in the NF150 chambers was typical for forests in the United States, but only 26% as high as that at Tanbark Flat in the Los Angeles Air Basin. We estimated that co-generated HNO 3 contributed 0.5% of the total N in current-year foliage of seedlings in the NF150 treatment. Irrigation treatment did not have a significant effect on throughfall chemistry except for a slightly greater decrease in throughfall pH in the well-watered plants compared with the drought-stressed plants in the pH 5.3 rain treatment in 1989. Absolute values for electrical conductivity and NO 3 − and NH 4 + content in throughfall tended to be higher with greater particulate dry deposition (45–55% removed versus 90% removed by filtration) in 1989 and 1990, but differences were not statistically significant.
    Type of Medium: Online Resource
    ISSN: 0045-5067 , 1208-6037
    Language: English
    Publisher: Canadian Science Publishing
    Publication Date: 1995
    detail.hit.zdb_id: 1473096-0
    SSG: 23
    SSG: 12
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  • 5
    Online Resource
    Online Resource
    Hindawi Limited ; 2002
    In:  The Scientific World JOURNAL Vol. 2 ( 2002), p. 122-130
    In: The Scientific World JOURNAL, Hindawi Limited, Vol. 2 ( 2002), p. 122-130
    Abstract: Measurement of ionic deposition in throughfall is a widely used method for measuring deposition inputs to the forest floor. Many studies have been published, providing a large database of throughfall deposition inputs to forests. However, throughfall collection and analysis is labor intensive and expensive because of the large number of replicate collectors needed and because sample collection and chemical analyses are required on a stochastic precipitation event-based schedule. Therefore we developed and tested a throughfall collector system using a mixed bed ion exchange resin column. We anticipate that this method will typically require only one to three samplings per year. With this method, bulk deposition and bulk throughfall are collected by a funnel or snow tube and ions are retained as the solution percolates through the resin column. Ions retained by the resin are then extracted in the same column with 2N KCl and analyzed for nitrate and ammonium. Deposition values in throughfall from conventional throughfall solution collectors and colocated ion exchange samplers were not significantly different during consecutive 3- and 4-month exposure periods at a high (Camp Paivika; 〉 35 kg N ha -1 year -1 ) and a low deposition (Barton Flats; 5–9 kg N ha -1 year -1 ) site in the San Bernardino Mountains in southern California. N deposition in throughfall under mature pine trees at Camp Paivika after 7 months of exposure was extremely high (87 and 92 kg ha -1 based on the two collector types) compared to Barton Flats (11 and 13 kg ha -1 ). A large proportion of the N deposited in throughfall at Camp Paivika occurred as fog drip, demonstrating the importance of fog deposition as an input source of N at this site. By comparison, bulk deposition rates in open areas were 5.1 and 5.4 kg ha -1 at Camp Paivika based on the two collector types, and 1.9 and 3.0 kg ha -1 at Barton Flats.
    Type of Medium: Online Resource
    ISSN: 1537-744X
    Language: English
    Publisher: Hindawi Limited
    Publication Date: 2002
    detail.hit.zdb_id: 2075968-X
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  • 6
    In: Ecological Applications, Wiley, Vol. 8, No. 3 ( 1998-08), p. 706-733
    Type of Medium: Online Resource
    ISSN: 1051-0761
    Language: English
    Publisher: Wiley
    Publication Date: 1998
    detail.hit.zdb_id: 2010123-5
    SSG: 12
    SSG: 23
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  • 7
    Online Resource
    Online Resource
    Wiley ; 1999
    In:  Journal of Environmental Quality Vol. 28, No. 3 ( 1999-05), p. 822-836
    In: Journal of Environmental Quality, Wiley, Vol. 28, No. 3 ( 1999-05), p. 822-836
    Abstract: We report streamwater nitrate (NO − 3 ) concentrations for December 1995 to September 1998 from 19 sampling sites across a N deposition gradient in the San Bernardino Mountains. Streamwater NO 3 concentrations in Devil Canyon (DC), a high‐pollution area, and in previously reported data from the San Gabriel Mountains 40 km northeast of Los Angeles, are the highest values reported in North America for undisturbed forest or shrub land watersheds. Concentrations in the primary stream draining western DC peaked at 350 µmol L −1 in December 1997 and minimum base flow NO − 3 concentrations were nearly always ≥80 µmol L −1 . In the San Gorgonio Wilderness (SGW), average NO − 3 concentrations in four streams along the southern transect (moderate N deposition), ranged from 10 to 37 µmol L −1 , while average NO − 3 concentrations were ≤0.7 µmol L −1 in seven streams along the northern transect (low N deposition). Peak NO − 3 concentrations in DC and in the SGW occurred after large winter storms, and a large spike in NO − 3 concentrations (10–370 µmol L −1 ) in SGW Streams 1 to 5 was observed after thundershower activity in July 1997. Streamwater export of NO 3 ‐N from Devil Canyon ranged from 3.6 to 11.6 kg ha −1 yr −1 during water years 1995 to 1998. This study further indicates that N emissions from fossil fuels and agriculture impact not only air quality, but also water quality from watersheds that are recipients of atmospheric N deposition.
    Type of Medium: Online Resource
    ISSN: 0047-2425 , 1537-2537
    Language: English
    Publisher: Wiley
    Publication Date: 1999
    detail.hit.zdb_id: 120525-0
    detail.hit.zdb_id: 2050469-X
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  • 8
    Online Resource
    Online Resource
    Wiley ; 2004
    In:  Journal of Environmental Quality Vol. 33, No. 6 ( 2004-11), p. 2007-2014
    In: Journal of Environmental Quality, Wiley, Vol. 33, No. 6 ( 2004-11), p. 2007-2014
    Abstract: Conventional throughfall collection methods are labor intensive and analytically expensive to implement at broad scales. This study was conducted to test an alternative approach requiring infrequent sample collection and a greatly reduced number of chemical analyses. The major objective of the study was to determine the feasibility of using ion exchange resin (IER) to measure N deposition in throughfall with field deployment periods of 3 to 12 mo. Nitrogen deposition measurements in bulk throughfall collected under pine ( Pinus sp.) canopies and in forest clearings were compared between co‐located conventional throughfall solution collectors and IER throughfall collectors using mixed bed IER columns. Deposition data were collected for 1 yr at a high deposition site (Camp Paivika, CP) and a relatively low one (Barton Flats, BF) in the San Bernardino Mountains in southern California: Annual throughfall deposition values (kg ha −1 of NH 4 –N + NO 3 –N) under large ponderosa pine trees ( Pinus ponderosa Laws.) were 145.8 and 143.9 at CP and 17.0 and 15.0 at BF according to the IER and conventional methods, respectively. Analogous values for bulk deposition in forest clearings were 15.6 and 12.3 at CP and 4.0 and 3.3 at BF. It was concluded that the IER collectors can be used for routine monitoring of deposition in throughfall and bulk deposition, provided that field blanks are used to account for background levels of N in the IER columns, which at times are slightly elevated, possibly from slow release of amine groups from the anion exchange resin during field exposures.
    Type of Medium: Online Resource
    ISSN: 0047-2425 , 1537-2537
    Language: English
    Publisher: Wiley
    Publication Date: 2004
    detail.hit.zdb_id: 120525-0
    detail.hit.zdb_id: 2050469-X
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  • 9
    Online Resource
    Online Resource
    Elsevier BV ; 1996
    In:  Forest Ecology and Management Vol. 82, No. 1-3 ( 1996-4), p. 211-230
    In: Forest Ecology and Management, Elsevier BV, Vol. 82, No. 1-3 ( 1996-4), p. 211-230
    Type of Medium: Online Resource
    ISSN: 0378-1127
    Language: English
    Publisher: Elsevier BV
    Publication Date: 1996
    detail.hit.zdb_id: 2016648-5
    detail.hit.zdb_id: 751138-3
    SSG: 23
    SSG: 12
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  • 10
    In: Canadian Journal of Forest Research, Canadian Science Publishing, Vol. 35, No. 6 ( 2005-06-01), p. 1464-1486
    Abstract: Net fluxes of nitrogen (N) mineralization and nitrification were measured in situ on a monthly basis for 3 years at a high (HN) and low (LN) N deposition site in the San Bernardino Mountains, California. Mean N mineralization fluxes in the forest floor and top 10 cm of mineral soil were 19.0 and 59.8 kg N·ha –1 ·year –1 at LN and HN, respectively. Mean net nitrification fluxes were 11.2 and 55.9 kg N·ha –1 ·year –1 at LN and HN, respectively. Relative nitrification (the percent N mineralized that was nitrified) was generally lower under Pinus ponderosa Dougl. ex P. & C. Laws. (or Pinus jeffreyi Grev. & Balf.) canopies than under Quercus kelloggii Newb. or open canopies. The rate of net N mineralization was the key factor for predicting the rate of net nitrification. Fertilization with 50 and 150 kg N·ha –1 at LN significantly increased the rates of net mineralization and net nitrification. At HN fertilization had no significant effect on net nitrification. We conclude that at low-deposition sites increased nitrification occurs in the short term in response to added N, but that sustained elevated net nitrification is driven by the accumulation of N-enriched litter and soil organic matter in conjunction with chronic throughfall N deposition inputs.
    Type of Medium: Online Resource
    ISSN: 0045-5067 , 1208-6037
    Language: English
    Publisher: Canadian Science Publishing
    Publication Date: 2005
    detail.hit.zdb_id: 1473096-0
    SSG: 23
    SSG: 12
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