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Carbon Sequestration and Nitrogen Status in Arenosols Following Afforestation or Following Abandonment of Arable Land

机译:植树造林或弃耕后荒漠土壤中的碳固存和氮素状况

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Over 600 000 ha of agricultural land on infertile soils (mainly Arenosols) are or soon will be abandoned in Lithuania. According to the resolution of the Kyoto Protocol, afforestation of this land could be relevant with the focus on carbon sequestration. The current study was carried out in a long-term permanent experiment in which arable Haplic Arenosols were afforested or before the abandonment were used as arable land during 25-ycar-long period. Soil chemical changes with an emphasis on organic carbon (C) and total nitrogen (N) pools, and the storages in ground vegetation cover and the roots were compared in 45-year-old Scots pine (Pinus sylvestris L.) plantations and abandoned (11 years ago) arable land. The former plaggic Ap horizon was less acid (by 1.3-1.9 pH units) and 2-3 times more saturated with mobile phosphorus and potassium compounds in plots on formerly fertilized abandoned arable land than in afforested with pine plantation plots. The total C pool at 100 cm mineral soil depth (including O horizons) in abandoned arable land (3.81 kg C m~(-2)) was 1.7 times less than in pine plantations (6.52 kg C m~(-2)), mainly because of C accumulation in the forest floor (2.24 kg C m~(-2). The differences in mineral horizons were not significant,although the root mass in mineral topsoil was more than 10 times larger in pine plantations, except the surface 0-2 cm layer of the former Ap horizon in which the C pool was 3 times larger in pine plantations (0.72 kg C M`(-2) than in abandoned arable land (0.22 kg C m~(-2)). Total soil N pools were at the same level (0.47-0.54 kg N m~(-2)) because the mineral soil to the depth of 100 cm contained 90% and more of N in both the abandoned arable land and the pine plantations. It was concluded that pine plantations better preserve C and N pools in mineral horizons of Haplic Arenosols, than abandoned arable land that was formerly intensively fertilized with conventional NPK fertilizers and farmyard manure as well.
机译:立陶宛即将或不久将废弃超过60万公顷的土地,主要是贫瘠的土壤(主要是槟榔)。根据《京都议定书》的决议,这片土地的植树造林可能与碳固存有关。当前的研究是在一项长期的永久性试验中进行的,在该试验中,对可耕种的哈普利人的槟榔进行了造林,或者在25年的漫长时期内将废弃的荒地用作耕地。比较了45年历史的苏格兰松树(Pinus sylvestris L.)人工林和弃置的土壤化学变化,重点是有机碳(C)和总氮(N)库,并比较了地面植被覆盖和根系的存储量。 11年前)耕地。与以前的松树人工林种植园相比,在以前施肥的废弃耕地中,以前贫瘠的Ap层的酸较少(以1.3-1.9 pH单位为单位),而移动性磷和钾化合物的饱和度高2-3倍。废弃耕地(3.81 kg C m〜(-2))在100 cm矿质土壤深度(包括O层)的总碳库比松树人工林(6.52 kg C m〜(-2))少1.7倍,主要是由于林地中碳的积累(2.24 kg C m〜(-2),矿物层位差异不显着,尽管除表层0外,松树人工林表层土的根系质量比根系大10倍以上。松树人工林(0.72 kg CM`(-2)的碳库比废弃的耕地(0.22 kg C m〜(-2))的C池大3倍,位于前Ap地平线的-2 cm层。结果表明,在废弃的耕地和松树人工林中,深度为100 cm的矿质土壤都含有90%或更多的N,因此水库处于相同水平(0.47-0.54 kg N m〜(-2))。与以前使用传统NPK肥料大量施肥的废弃耕地相比,松树人工林在Haplic Arenosols的矿藏中更好地保​​存了C和N库。以及农家肥。

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