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Effect of clear cutting on nutrient fluxes in a subalpine forest at Fraser, Colorado

机译:科罗拉多州弗雷泽的亚高山森林中,砍伐对养分通量的影响

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Nutrient fluxes were investigated on a forested anda clearcut plot in a mixed conifer high elevation (2900 m) forest at theFraser Experimental Forest in Fraser, Colorado, USA. Plots were locatedon a coarse loamy mixed Dystric Cryochrept with relatively high base saturation(30-90%) and underlain by an impermeable clay subsoil. Following harvestin late 1984, annual mean NO3 concentrations of 195 to 198 μmol l-1 wereobserved from 1988 through 1990 and concentrations were still above referencelevels in 1993. Total nitrogen loss attributable to leaching followingharvest was estimated at 48kg ha-1 over 8 years. Over this same period,atmospheric nitrogen inputs exceeded annual outflow of NH4 plus NO3 fromthe control plots by approximately 11 kg N ha-1. A slight enrichment OfSO4 and Cl was observed from the harvested plot in 1986 but concentrationslater fell below control plot levels, apparently due to dilution by theincreased discharge from the harvested plot which was three to four timesthat from the control plot. Elevated Ca, Mg, and Na concentrations followeda similar pattern to NO3 due to exchange reactions, while a depressionin alkalinity of about one-third the amount of NO3 found was also observed.Enrichment of K occurred primarily in water collected at less than 1 mdepth. Increases in base cation loss due to leaching after harvest wereabout twice the amount that can be accounted for by the increased fluxof NO3, SO4, and Cl anions. The excess reflects the increased water fluxand consequent leaching of base cations in association with HCO3 and organicanions.
机译:在美国科罗拉多州弗雷泽(Fraser)的弗雷泽实验森林(Fraser Experiment Forest)的针叶树高海拔混合森林(2900 m)的密林和伐木区调查了养分通量。地块位于具有较高基饱和度(30-90%)的粗壤质混合型Dystric Cryochrept上,并被不可渗透的粘土底土覆盖。在1984年末收获之后,从1988年到1990年观察到的年平均NO 3 浓度为195至198μmoll -1 ,1993年的浓度仍高于参考水平。可归因于总氮损失在8年中,估计收获后的淋溶量为48kg ha -1 。在同一时期,大气氮输入量每年比对照区的NH 4 加NO 3 高出约11 kg N ha -1 。 1986年在收割的土地上观察到SO 4 和Cl的少量富集,但浓度后来下降到对照土地的水平以下,这显然是由于收割土地排放量的增加所造成的稀释,这是对照土地的三到四倍。情节。 由于交换反应,Ca,Mg和Na浓度升高与NO 3 相似,而碱度下降约NO 3 三分之一钾的富集主要发生在深度小于1 m的水中。收获后浸出导致的碱阳离子损失增加量约为NO 3 ,SO 4 和Cl阴离子通量增加可解释的增加量的两倍。过量反映出水通量的增​​加以及随之而来的碱阳离子与HCO 3 和有机阴离子的浸出。

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