Increased nitrogen leaching following soil freezing is due to decreased root uptake in a northern hardwood forest

被引:117
作者
Campbell, John L. [1 ]
Socci, Anne M. [2 ]
Templer, Pamela H. [2 ]
机构
[1] US Forest Serv, No Res Stn, USDA, Durham, NH 03824 USA
[2] Boston Univ, Dept Biol, Boston, MA 02215 USA
基金
美国国家科学基金会; 美国安德鲁·梅隆基金会;
关键词
climate change; root uptake; snow; soil frost; soil solution; stable isotopes; NORTHEASTERN UNITED-STATES; BROOK-EXPERIMENTAL-FOREST; NUTRIENT-UPTAKE CAPACITY; SNOW DEPTH; CATSKILL MOUNTAINS; FUTURE CHANGES; NITRATE UPTAKE; CLIMATE-CHANGE; NEW-HAMPSHIRE; INTACT ROOTS;
D O I
10.1111/gcb.12532
中图分类号
X176 [生物多样性保护];
学科分类号
090705 ;
摘要
The depth and duration of snow pack is declining in the northeastern United States as a result of warming air temperatures. Since snow insulates soil, a decreased snow pack can increase the frequency of soil freezing, which has been shown to have important biogeochemical implications. One of the most notable effects of soil freezing is increased inorganic nitrogen losses from soil during the following growing season. Decreased nitrogen retention is thought to be due to reduced root uptake, but has not yet been measured directly. We conducted a 2-year snow-removal experiment at Hubbard Brook Experimental Forest in New Hampshire, USA to determine the effects of soil freezing on root uptake and leaching of inorganic nitrogen simultaneously. Snow removal significantly increased the depth of maximal soil frost by 37.2 and 39.5 cm in the first and second winters, respectively (P < 0.001 in 2008/2009 and 2009/2010). As a consequence of soil freezing, root uptake of ammonium declined significantly during the first and second growing seasons after snow removal (P = 0.023 for 2009 and P = 0.005 for 2010). These observed reductions in root nitrogen uptake coincided with significant increases in soil solution concentrations of ammonium in the Oa horizon (P = 0.001 for 2009 and 2010) and nitrate in the B horizon (P < 0.001 and P = 0.003 for 2009 and 2010, respectively). The excess flux of dissolved inorganic nitrogen from the Oa horizon that was attributable to soil freezing was 7.0 and 2.8 kg N ha(-1) in 2009 and 2010, respectively. The excess flux of dissolved inorganic nitrogen from the B horizon was lower, amounting to 1.7 and 0.7 kg N ha(-1) in 2009 and 2010, respectively. Results of this study provide direct evidence that soil freezing reduces root nitrogen uptake, demonstrating that the effects of winter climate change on root function has significant consequences for nitrogen retention and loss in forest ecosystems.
引用
收藏
页码:2663 / 2673
页数:11
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