...
首页> 外文期刊>Water, Air, and Soil Pollution >TEMPORAL AND SPATIAL VARIATIONS IN SOIL WATER CHEMISTRY AT THREE ACID FOREST SITES
【24h】

TEMPORAL AND SPATIAL VARIATIONS IN SOIL WATER CHEMISTRY AT THREE ACID FOREST SITES

机译:三种酸林地土壤水化学的时空变化

获取原文
获取原文并翻译 | 示例
   

获取外文期刊封面封底 >>

       

摘要

As acid deposition declines, recovery from acidification is delayed by the fact that the soil processes that earlier buffered against acidification are now being reversed. Monitoring of within catchment processes is thus desirable. However, soil sampling is destructive and not suitable for long-term monitoring at a single site, whereas sampling of soil water with suction lysimeters may be more suitable. In this paper we evaluate 8-11 years of soil water chemistry from E- and B-horizons in three acid forest soil plots within monitored catchments. Five years of sampling also included the C-horizon. To our knowledge, this is the first long-term lysimeter study including the E-horizon showing recovery from acidification, and one of few studies including the B-horizon. Soil water concentrations of SO_4 decreased significantly between -9.5 and -1.4 μeq L~(-1) yr~(-1), with much higher rates of change at two southern sites compared to a northern site, where levels and changes of deposition were lower. The average annual bulk deposition of S ranged between 3 kg S ha~(-1) at the northernmost site to 11 kg S ha~(-1) at the southernmost site. The SO_4 decline in E-horizons was smaller than the decline in deposition, which indicated leaching of SO_4 from the O-horizon. At the two southern sites, a weaker decline in SO_4 in the B-horizon compared to the E-horizon indicated desorption of SO_4. The negative trends in SO_4 were to a large extent balanced by decreases in base cations but there were also tendencies of recovery from acidification in soil solution at the southern sites by increasing pH and ANC. However, these were contradicted by increasing Al concentrations. A high influence of marine salts in the early 1990s may have delayed the recovery. Decreasing trends of the Ca/(H~+)~2 ratio in the soil solution, most pronounced at one of the southern sites, suggested that the soils were becoming more acidic, although the soil solution tended to recover.
机译:随着酸沉降的减少,由于早先被缓冲以抵抗酸化的土壤过程现在被逆转,这一事实延迟了酸化的恢复。因此,需要对集水区内的过程进行监控。但是,土壤采样具有破坏性,不适合在单个站点进行长期监控,而采用吸气式渗漏计采样土壤水可能更适合。在本文中,我们评估了受监测流域内三个酸性森林土壤小区中E和B地平线的8-11年土壤水化学性质。五年的采样还包括C地平线。据我们所知,这是第一个长期的溶渗仪研究,包括显示从酸化中恢复的E-水平仪,也是包括B-水平仪在内的少数研究之一。 SO_4的土壤水浓度在-9.5和-1.4μeqL〜(-1)yr〜(-1)之间显着降低,与北部地区相比,两个南部地区的变化率要高得多,而北部地区的沉积水平和沉积物变化是降低。 S的年平均沉积量在最北端的3 kg S ha〜(-1)到最南端的11 kg S ha〜(-1)之间。 E_horizo​​n中SO_4的下降小于沉积的下降,这表明SO_4从O-horizo​​n中浸出。在两个南部站点,与E地平线相比,B地平线中SO_4的下降幅度较小,表明SO_4的解吸。 SO_4的负趋势在很大程度上与碱性阳离子的减少相平衡,但在南部地区,pH值和ANC的增加也使土壤溶液酸化有恢复的趋势。但是,这些与铝浓度的增加矛盾。 1990年代初期,海盐的巨大影响可能延迟了恢复。土壤溶液中Ca /(H〜+)〜2比值的下降趋势(在南部地区之一最为明显)表明,尽管土壤溶液有恢复的趋势,但土壤变得越来越酸性。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号