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First rotation biomass production and nutrient cycling within short-rotation coppice willow plantations in Saskatchewan, Canada

机译:加拿大萨斯喀彻温省短轮转杨柳人工林中首次轮作生物量生产和养分循环

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摘要

Although numerous studies have quantified different social, economic, energetic, and environmental benefits associated with short-rotation coppice (SRC) willow plantations, comprehensive assessments of nutrient cycling are rare. The objective of this study was to examine the biomass production and attendant biogeochemical cycling of nitrogen (N), phosphorus (P), potassium (K), sulphur (S), calcium (Ca), and magnesium (Mg) during the initial four-year rotation of six willow varieties grown at fourudlocations along a 500 km north-south pedoclimatic gradient within Saskatchewan, Canada. Nutrient budgets consisted of quantifying various nutrient inputs (e.g., atmospheric deposition and soil mineral weathering), outputs (e.g., fine and coarse root biomass, leaf biomass, harvested biomass, leaching, and denitrification), and transfers (e.g., soil organic matter mineralization, canopy exchange, leaf litteruddecomposition, and fine root turnover) associated with the plant available soil nutrient pool. Total above- and below-ground production during the rotation was approximately 40 Mg ha-1, with calculated soil nutrient budget deficits (i.e., nutrient outputs > inputs + transfers) of 17, 39, 112, 271, and 74 kg ha-1 for N, P, K, Ca, and Mg, respectively, averaged across the varieties and sites, but a soil S surplus of 60 kg ha-1. While soil nutrient budget deficits varied among sites, there were no significant differences (P >0.05) among willow varieties. Despite the relatively low nutrient-demanding nature of willow and negligible leaching or denitrification losses, nutrient export in harvested biomass over multiple rotations will require soil nutrient amendments to maintain SRC willow productivity, particularly N and P, albeit a fraction of the amount required for annual agronomic crops.
机译:尽管许多研究已经量化了与短轮距小灌木林(SRC)柳树人工林相关的不同的社会,经济,活力和环境效益,但对养分循环的综合评估却很少。这项研究的目的是检查在最初的四个阶段中氮(N),磷(P),钾(K),硫(S),钙(Ca)和镁(Mg)的生物量生产和伴随的生物地球化学循环在加拿大萨斯喀彻温省沿南北500 km的古气候梯度,在四个位置处生长的六个柳树品种的年轮换。营养预算包括量化各种营养输入(例如,大气沉积和土壤矿物风化),输出(例如,细根和粗根生物量,叶片生物量,收获的生物量,浸出和反硝化)和转移(例如,土壤有机质矿化) ,冠层交换,叶片凋落物分解和细根周转)与植物可用的土壤养分库相关。轮作期间地上和地下的总产量约为40 Mg ha-1,计算出的土壤养分预算赤字(即养分输出>投入+转移)为17,39、112、271和74 kg ha-1 N,P,K,Ca和Mg分别在不同品种和产地的平均值,但土壤S剩余量为60 kg ha-1。虽然不同地点的土壤养分预算赤字有所不同,但柳树品种之间没有显着差异(P> 0.05)。尽管柳树对养分的需求量相对较低,淋溶或反硝化损失可忽略不计,但经过多次轮作,收获的生物量中的养分出口仍需要改良土壤养分以维持SRC柳树的生产力,尤其是氮和磷,尽管只是每年所需量的一小部分农作物。

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