首页> 外文期刊>Hydrology and Earth System Sciences >Long-term changes in precipitation and stream water chemistry in small forest and moorland catchments at Beddgelert Forest, north Wales
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Long-term changes in precipitation and stream water chemistry in small forest and moorland catchments at Beddgelert Forest, north Wales

机译:北威尔士贝德格勒森林的小森林和高沼地流域降水和溪流水化学的长期变化

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Changes in the chemistry of bulk precipitation and stream water between 1982 and 2000 are described for small moorland and forest catchments located within Beddgelert Forest in north Wales. Two forest catchments were partially clearfelled in 1984 (D2; 68% and D4; 28%) whilst a third (D3) remained as an unfelled control until autumn / winter 1998/99 when partial felling took place in the headwaters. Over the monitoring period, the annual mean pH of bulk precipitation increased from 4.6 to 5.1 whilst the annual mean non-seasalt sulphate concentration decreased from 0.53 mg S l-1 in 1985 to 0.24 mg S l-1 in 2000. Since 1985, the annual wet deposition flux of non-seasalt sulphur decreased by 50% to 8.4 kg S ha-1 yr–1 in 2000. Annual mean inorganic nitrogen concentrations and annual wet deposition fluxes have remained relatively unchanged since 1982. The decrease in atmospheric sulphur deposition is reflected by decreased annual mean concentrations of non-seasalt sulphur, acidity, aluminium and calcium in all four streams irrespective of clearfelling activities. Annual variations in nitrate-N and potassium concentrations in the forest streams, largely determined by pulses of leaching following forest clearance, had no effect on stream acidity. In common with UK upland catchments, annual mean concentrations of dissolved organic carbon have increased from about 1 mg C l-1 in 1985 to between 1.5 and 2 mg C l-1 in 2000, although there is considerable year to year variability. Two boreholes drilled adjacent to catchments D3 and D4 have confirmed the presence of alkaline, base rich groundwater at Beddgelert. Although the boreholes are only 150 m apart, there are large differences in chemistry suggesting that different groundwater reservoirs have been intercepted providing further evidence of the complexity and heterogeneity of groundwater systems in upland catchments. style="line-height: 20px;">Keywords: acid deposition, acidification, recovery, forestry, clearfelling, trends, Beddgelert, streams, rainfall
机译:描述了1982年至2000年之间威尔士北部贝德盖勒特森林内的小高沼地和森林集水区的总体降水和溪流水化学变化。 1984年,两个森林集水区被部分砍伐(D2; 68%,D4; 28%),而第三个(D3)作为未砍伐的森林保持原状,直到1998/99秋/冬季源头部分砍伐。在监测期内,大降水的年平均pH从4.6增加到5.1,而非海盐硫酸盐的年平均浓度从1985年的0.53 mg S l -1 下降到0.24 mg S l -1 。自1985年以来,2000年非海盐硫的湿沉降通量下降了50%,降至8.4 kg S ha -1 yr-1。年平均无机自1982年以来,氮的浓度和年湿沉积通量一直保持相对不变。大气中硫的沉积减少反映了所有四种流中非海盐硫,酸度,铝和钙的年平均浓度的降低,而与清除采伐活动无关。森林溪流中硝酸盐氮和钾浓度的年变化主要由森林清除后的浸出脉冲决定,对溪流酸度没有影响。与英国陆地集水区一样,溶解有机碳的年平均浓度从1985年的约1 mg C l -1 增加到1.5至2 mg C l -1 尽管在2000年之间存在很大的年度差异,在D3和D4集水区附近钻了两个钻孔,证实在Beddgelert有碱性的,富含碱的地下水。尽管钻孔仅相距150 m,但化学差异很大,这表明已拦截了不同的地下水库,为陆上流域地下水系统的复杂性和非均质性提供了进一步的证据。 style =“ line-height :20px;“> 关键字:酸沉降,酸化,恢复,林业,清除伐木,趋势,贝德格勒特,溪流,降雨

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