Momen Bahram, Behling Shawna J, Lawrence Greg B, Sullivan Joseph H
Environmental Science and Technology Department, University of Maryland, College Park, Maryland, United States of America.
Plant Science and Landscape Architecture Department, University of Maryland, College Park, Maryland, United States of America.
PLoS One. 2015 Aug 20;10(8):e0136148. doi: 10.1371/journal.pone.0136148. eCollection 2015.
Decline of sugar maple in North American forests has been attributed to changes in soil calcium (Ca) and nitrogen (N) by acidic precipitation. Although N is an essential and usually a limiting factor in forests, atmospheric N deposition may cause N-saturation leading to loss of soil Ca. Such changes can affect carbon gain and growth of sugar maple trees and seedlings. We applied a 22 factorial arrangement of N and dolomitic limestone containing Ca and Magnesium (Mg) to 12 forest plots in the Catskill Mountain region of NY, USA. To quantify the short-term effects, we measured photosynthetic-light responses of sugar maple mature trees and seedlings two or three times during two summers. We estimated maximum net photosynthesis (An-max) and its related light intensity (PAR at An-max), apparent quantum efficiency (Aqe), and light compensation point (LCP). To quantify the long-term effects, we measured basal area of living mature trees before and 4 and 8 years after treatment applications. Soil and foliar chemistry variables were also measured. Dolomitic limestone increased Ca, Mg, and pH in the soil Oe horizon. Mg was increased in the B horizon when comparing the plots receiving N with those receiving CaMg. In mature trees, foliar Ca and Mg concentrations were higher in the CaMg and N+CaMg plots than in the reference or N plots; foliar Ca concentration was higher in the N+CaMg plots compared with the CaMg plots, foliar Mg was higher in the CaMg plots than the N+CaMg plots; An-max was maximized due to N+CaMg treatment; Aqe decreased by N addition; and PAR at An-max increased by N or CaMg treatments alone, but the increase was maximized by their combination. No treatment effect was detected on basal areas of living mature trees four or eight years after treatment applications. In seedlings, An-max was increased by N+CaMg addition. The reference plots had an open herbaceous layer, but the plots receiving N had a dense monoculture of common woodfern in the forest floor, which can impede seedling survival.
北美森林中糖枫的衰退被归因于酸性降水导致的土壤钙(Ca)和氮(N)的变化。尽管氮是森林中一种必需且通常是限制因素,但大气氮沉降可能导致氮饱和,进而导致土壤钙流失。这些变化会影响糖枫树木和幼苗的碳获取和生长。我们在美国纽约州卡茨基尔山区的12个森林地块上采用了氮与含钙和镁(Mg)的白云石石灰石的二因素组合处理。为了量化短期影响,我们在两个夏天对糖枫成年树和幼苗的光合光响应进行了两到三次测量。我们估计了最大净光合作用(An-max)及其相关光强(An-max时的光合有效辐射)、表观量子效率(Aqe)和光补偿点(LCP)。为了量化长期影响,我们在处理前以及处理后4年和8年测量了活成年树的基部面积。还测量了土壤和叶片化学变量。白云石石灰石增加了土壤Oe层中的钙、镁和pH值。与接受氮处理的地块相比,接受钙镁处理的地块B层中的镁含量增加。在成年树中,钙镁处理地块和氮+钙镁处理地块的叶片钙和镁浓度高于对照或氮处理地块;氮+钙镁处理地块的叶片钙浓度高于钙镁处理地块,钙镁处理地块的叶片镁含量高于氮+钙镁处理地块;由于氮+钙镁处理,An-max达到最大值;添加氮会降低Aqe;单独的氮或钙镁处理会使An-max时的光合有效辐射增加,但两者组合时增加幅度最大。在处理后4年或八年,未检测到对活成年树基部面积的处理效果。在幼苗中,添加氮+钙镁会增加An-max。对照地块有开阔的草本层,但接受氮处理的地块在森林地面有密集的单一种植的普通木贼,这可能会阻碍幼苗存活。