Albaugh Timothy J, Allen H Lee, Fox Thomas R
Department of Forestry and Environmental Resources, North Carolina State University, Raleigh, NC 27695-8008, USA.
Tree Physiol. 2008 Jul;28(7):1083-98. doi: 10.1093/treephys/28.7.1083.
We quantified nitrogen (N), phosphorus (P), potassium (K), calcium (Ca) and magnesium (Mg) content, use (nutrient amount for one growth year), retranslocation (nutrients recycled before foliage senescence), uptake (use minus retranslocation), volume production per unit of uptake and fertilizer-uptake efficiency (percent applied taken up) in a 2 x 2 (nutrient and water) factorial experiment replicated four times in an 8-year-old loblolly pine (Pinus taeda L.) stand growing on a nutrient-poor sandy soil in Scotland County, North Carolina, USA. Over 14 years, we applied 1140, 168, 393, 168 and 146 kg ha(-1) of elemental N, P, K, Ca and Mg fertilizer, respectively, and an average of 710 mm year(-1) of irrigation. All plots received complete vegetation control. Fertilization about doubled tissue N, P, K and Mg contents at age 21, whereas irrigation resulted in smaller increases in nutrient contents. Maximum annual uptake was 101, 9.3, 44, 37 and 13 kg ha(-1) year(-1) and volume production per unit of nutrient uptake was 0.35, 3.5, 0.66, 1.1 and 3.1 m(3) kg(-1), for N, P, K, Ca and Mg, respectively. Irrigated plots had greater volume production per unit of N, P, K and Mg uptake than control plots, likely because irrigation allowed photosynthesis to continue during dry periods. Fertilized plus irrigated plots had less volume production per unit of these elements than the fertilized plots either because nutrient uptake exceeded the requirement for optimum growth or because available water (rainfall plus irrigation) was insufficient for the leaf area achieved with fertilization. At age 19, fertilizer-uptake efficiencies for N, P, K, Ca and Mg were 53, 24, 62, 57 and 39%, respectively, and increased with irrigation to 68, 36, 78, 116 and 55%, respectively. The scale of fertilizer uptake was likely a result of low native site nutrient availability, study longevity, measurement of all tissue components on site, a comprehensive assessment of coarse roots, and the 3-m rooting depth. Ecosystem nitrogen retention (applied nitrogen found in living plant material, litter fall and soil to 150-cm depth) was estimated at 79% at age 17, a value that would likely be greater when including soil nitrogen to rooting depth and calculating retention at age 21 when the study ended. The ecosystem retention value provides evidence that intensive site resource management can be accomplished with low likelihood of applied materials moving offsite.
在美国北卡罗来纳州苏格兰县一片生长在贫瘠沙质土壤上的8年生火炬松(Pinus taeda L.)林分中,我们开展了一项2×2(养分和水分)析因试验,并重复4次,对氮(N)、磷(P)、钾(K)、钙(Ca)和镁(Mg)的含量、用量(一个生长年的养分量)、再转运(叶片衰老前回收的养分)、吸收量(用量减去再转运量)、单位吸收量的材积产量以及肥料吸收效率(吸收的施用肥料百分比)进行了量化。在14年时间里,我们分别施用了1140、168、393、168和146 kg·ha⁻¹的单质氮、磷、钾、钙和镁肥料,平均每年灌溉710 mm。所有样地都进行了完全的植被控制。施肥使21年生时组织中的氮、磷、钾和镁含量增加了约一倍,而灌溉使养分含量的增加幅度较小。氮、磷、钾、钙和镁的最大年吸收量分别为101、9.3、44、37和13 kg·ha⁻¹·年⁻¹,单位养分吸收量的材积产量分别为0.35、3.5、0.66、1.1和3.1 m³·kg⁻¹。灌溉样地单位氮、磷、钾和镁吸收量的材积产量高于对照样地,这可能是因为灌溉使光合作用在干旱时期得以持续。施肥加灌溉样地这些元素的单位材积产量低于施肥样地,原因可能是养分吸收超过了最佳生长所需,或者是有效水分(降雨加灌溉)不足以维持施肥后达到的叶面积。19年生时,氮、磷、钾、钙和镁的肥料吸收效率分别为53%、24%、62%、57%和39%,灌溉后分别提高到68%、36%、78%、116%和55%。肥料吸收规模可能是由于原生立地养分有效性低、研究时间长、对现场所有组织成分进行测量、对粗根进行全面评估以及3米的生根深度。生态系统氮保留量(在活植物材料、凋落物和150厘米深度土壤中发现的施用氮)在17年生时估计为79%,如果将土壤氮计算到生根深度并在研究结束时计算21年生时的保留量,这个值可能会更大。生态系统保留值证明,通过强化立地资源管理,施用材料移出场地的可能性较低。