首页> 外文期刊>Forest Ecology and Management >Variation in soil carbon in pine plantations and implications for monitoring soil carbon stocks in relation to land-use change and forest site management in New Zealand.
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Variation in soil carbon in pine plantations and implications for monitoring soil carbon stocks in relation to land-use change and forest site management in New Zealand.

机译:新西兰人工林土壤碳的变化及其对监测土壤碳储量与土地利用变化和森林场址管理的关系。

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Various methods were assessed to determine the impact of forest harvesting on mineral soil carbon (C) in Pinus radiata stands at Puruki catchment in the central North Island of New Zealand. Previous work at this site reported a reduction in soil carbon of 3.6 Mg ha-1 in the top 0.1 m over one 23-year rotation of pine on improved pasture [Beets, P.N., Oliver, G.R., Clinton, P.W., 2002. Soil carbon protection in podocarp/hardwood forest, and the effects of conversion to pasture and exotic pine forest. J. Environ. Pollut. 116, S63-S73]. In this study, by sampling before and after harvesting, a further reduction of 3.1 Mg ha-1 (significant at P=0.05) in mineral soil carbon stocks to 0.1 m depth was found to be associated with harvesting disturbance. However, less intensive sampling was unable to detect any significant harvesting effects in depths down to 2 m. Variation between plots was large, and it was estimated that to detect a 10% change in carbon content with 95% confidence 19 permanent plots would be required for 0-0.1 m depth and 40 permanent plots required to detect changes to 1 m depth. Soil C content to 1 m depth in Puruki Rua subcatchment was estimated to average between 143 and 164 Mg ha-1. In two paired-site studies comparing pasture with second rotation pine, the difference between land-uses in mineral soil C content to 0.1 m depth was 19.6 Mg ha-1 in volcanic soil at Kaingaroa and 8.5 Mg ha-1 in high clay activity soil at Ngaumu. Significant differences in mineral soil C between pine and pasture was found with cumulative depth down to 2 m, well below the rooting depth of pasture, which suggests that historic factors overshadowed influences of the current land-use and can account for the difference in soil carbon. At Kaingaroa, variability in soil carbon content was high at all depths measured, and to detect a 10% difference in soil carbon content with 95% confidence approximately 60 pits measured to 1 m depth would be required.
机译:评估了各种方法以确定森林砍伐对新西兰北岛中部普鲁基河流域辐射松林地中矿质土壤碳(C)的影响。该地点以前的工作报告说,在改良的牧场上,每旋转23年,松树旋转23年,顶部0.1 m的土壤碳减少3.6 Mg ha-1 [甜菜,PN,Oliver,GR,克林顿,PW,2002。土壤碳对罗汉松/阔叶林的保护,以及转为牧场和外来松林的影响。 J.环境。污染116,S63-S73]。在这项研究中,通过在收获之前和之后进行采样,发现矿物质土壤碳储量进一步减少3.1 Mg ha-1(在P = 0.05时显着)至0.1 m深度与收获扰动有关。但是,强度较低的采样无法检测到2 m以内的任何重大收获效果。地块之间的差异很大,据估计,要以95%的可信度检测碳含量的10%变化,则0-0.1 m深度需要19个永久性地块,而检测1m深度的变化则需要40个永久性地块。 Puruki Rua小流域1 m深的土壤碳含量估计平均为143至164 Mg ha-1。在两个牧场对比第二次旋转松的成对研究中,矿床土壤中C含量至0.1 m深度的土地利用差异在Kaingaroa的火山土壤中为19.6 Mg ha-1,在高粘土活性土壤中为8.5 Mg ha-1在N松树和牧场之间的矿质土壤碳存在显着差异,累积深度低至2 m,远低于牧场的生根深度,这表明历史因素掩盖了当前土地利用的影响,并可以解释土壤碳的差异。在Kaingaroa,在所有测得的深度处土壤碳含量的变化都很大,要在95%置信度下检测10%的土壤碳含量差异,就需要在1 m深度处测量大约60个坑。

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