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首页> 外文期刊>Forestry >Short-term effects of lime application on soil properties and fine-root characteristics for a 9-year-old Sitka spruce plantation growing on a deep peat soil
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Short-term effects of lime application on soil properties and fine-root characteristics for a 9-year-old Sitka spruce plantation growing on a deep peat soil

机译:石灰对深泥炭土壤中生长的9年龄Sitka云杉人工林土壤特性和细根特性的短期影响

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Short-term effects of lime application on a 9-year-old Sitka spruce (Picea sitchensis (Bong.) Carr.)) stand planted on a deep blanket peat soil were investigated. Ground limestone was applied at three rates: 7.5 (L-1), 15.0 (L-2) and 22.5 t ha(-1) (L-3) Plus a control (L-0). The peat was sampled on the first and second growing seasons after lime application. Soil properties were examined for the litter layer and three depths of the peat profile at 5 cm intervals, while fine root (<2 mm in diameter) characteristics were examined for the litter layer and top 5 cm of the peat profile. Soil water pH and minerals were determined for the second growing season only. Liming decreased the concentration of N in the litter layer and top 10 cm of the peat profile at the first growing season. In contrast, concentration of this element in the litter layer and top 15 cm of the peat profile was increased by liming at the second growing season. Concentration of C in the liner and below-litter layers was unaffected by liming on both sampling occasions. Lime application increased the soil water pH and concentrations of P, Ca, B and NH4+-N in the soil water. Concentration of Mg in the soil water was increased by liming only for the L-2 and L-3 plots. The soil water had a high concentration of NO3--N in the L-1 plots and low concentrations of Cu and NO3--N in the L-3 plots compared with unlimed plots. Mean fine-root dry weight and length were 0.21 g l(-1) and 177 cm l(-1), respectively. Dead fine roots were present in small amounts and only in limed plots at the first growing season. Distribution of fine roots was restricted to the litter layer and the top 5 cm of the peat profile with the majority in the litter layer. Fine-root dry weight was unaffected by liming at the first growing season, but increased by 40, 93 and 127 per cent in the L-1, L-2 and L-3 plots, respectively, at the second growing season. Fine-root length in the L-1 plots was 36 per cent lower than that in the L-0 plots at the first growing season. Length of fine roots was increased by 93, 131 and 137 per cent in the L-1, L-2 and L-3 plots, respectively, at the second growing season. The L-1 Plots had a low number of long root tips (>1 cm in length) in the litter layer compared with the L-0 plots at the first growing season, while numbers of short (<1 cm in length) and long root tips were increased by liming at the second growing season. Number of root tips per fine root length (no. cm(-1)) in the litter layer and number of total root tips per root length were increased in the L-1 and L-2 plots. Concentrations of P, K, Ca and Mg in the live fine roots were increased by liming at the first growing season. Liming increased the concentration of Ca and decreased the concentrations of Mn and Al in live fine roots at the second growing season. It seems that fine-root minerals are changed by liming and Such changes are dependent on the time interval following lime application to the peat soil.
机译:研究了在深厚的盖层泥炭土上种植的9岁Sitka云杉(Picea sitchensis(Bong。)Carr。)的短期施用石灰的效果。以三种比率施用研磨的石灰石:7.5(L-1),15.0(L-2)和22.5 t ha(-1)(L-3)加上对照(L-0)。在施用石灰后的第一个和第二个生长季节取样泥炭。以5 cm的间隔检查垃圾层和三个深度的泥炭剖面的土壤特性,同时检查垃圾层和泥炭剖面的顶部5 cm的细根(直径<2 mm)特征。仅在第二个生长季节确定土壤水的pH值和矿物质。石灰在第一个生长季节降低了凋落物层和泥炭剖面顶部10 cm的N浓度。相反,在第二个生长季节通过撒石灰增加了该元素在垫料层和泥炭剖面顶部15 cm的浓度。两次采样时,石灰对衬里和垫料下层中C的浓度均没有影响。石灰的施用增加了土壤水的pH值以及土壤水中P,Ca,B和NH4 + -N的浓度。仅通过在L-2和L-3样地上撒石灰可以增加土壤水中Mg的浓度。与未限制地块相比,L-1地块中的土壤水中NO3--N浓度高,而L-3地块中的Cu和NO3--N浓度低。平均细根干重和长度分别为0.21 g l(-1)和177 cm l(-1)。死细根少量存在,仅在第一个生长季节的灰土地上。细根的分布仅限于垫料层和泥炭剖面的顶部5 cm,其中大部分位于垫料层。在第一个生长季节,细根干重不受石灰的影响,但在第二个生长季节,L-1,L-2和L-3地块分别增加了40%,93%和127%。在第一个生长季节,L-1地块的细根长度比L-0地块的细根长度低36%。在第二个生长季节,L-1,L-2和L-3地块的细根长度分别增加了93%,131%和137%。与第一个生长季节的L-0地块相比,L-1地块的凋落物层中的长根尖(长度> 1厘米)数量少,而短地(长度<1厘米)和长根地块数量少在第二个生长季节通过撒石灰增加根尖。在L-1和L-2图中,凋落物层中每细根长度(根数cm(-1))的根尖数和每根长度的总根尖数均增加。在第一个生长季节通过撒石灰增加了活细根中P,K,Ca和Mg的含量。石灰在第二个生长季节增加了活细根中Ca的浓度,降低了Mn和Al的浓度。看来细根矿物是通过石灰改变的,这种变化取决于石灰在泥炭土壤中施用后的时间间隔。

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