Borken Werner, Xu Yi-Jun, Beese Friedrich
Department of Soil Ecology, BITOK, University of Bayreuth, Dr. Hans-Frisch-Strasse 1-3, 95440 Bayreuth, Germany.
J Environ Qual. 2004 Jan-Feb;33(1):89-98. doi: 10.2134/jeq2004.8900.
The objective of this study was to assess the effect of compost application on soil respiration and dissolved organic carbon (DOC) output of nutrient-depleted forest soils. An amount of 6.3 kg m(-2) mature compost was applied to the forest floor of European beech (Fagus sylvatica L.), Norway spruce (Picea abies Karst.), and Scots pine (Pinus sylvestris L.) stands at Soiling and Unterlüss, Germany. Cumulative soil respiration significantly increased by 499 g C m(-2) in the spruce stand at Unterlüss and by 274 g C m(-2) in the beech stand at Soiling following compost application whereas soil respiration of the other four stands was not affected. The increases in soil respiration of the two stands were explained by improved microbial decomposition of soil organic matter. The DOC concentrations and fluxes in throughfall and seepage water at 10- and 100-cm depths were determined from August 1997 to March 2000. In the control plots, cumulative DOC outputs at 10 cm ranged between 57 and 95 g C m(-2), with the highest rates in the pine stands. Compost treatment significantly increased cumulative DOC outputs by 31 to 69 g C m(-2) at 10 cm and by 0.3 to 6.6 g C m(-2) at 100 cm. The mineral soils between the 10- and 100-cm depths acted as significant sinks for DOC, as shown by much lower cumulative outputs at 100 cm of 3 to 11 g C m(-2) in the control and 6 to 16 g C m(-2) in the compost plots. Our results suggest that a single, moderate application of mature compost to nutrient-depleted forest soils has little effect on C losses to the atmosphere and ground water.
本研究的目的是评估施用堆肥对养分贫瘠森林土壤的土壤呼吸和溶解有机碳(DOC)输出的影响。在德国索林和 Unterlüss,将6.3 kg m(-2) 的成熟堆肥施用于欧洲山毛榉(Fagus sylvatica L.)、挪威云杉(Picea abies Karst.)和苏格兰松(Pinus sylvestris L.)林分的林地。施用堆肥后,Unterlüss 的云杉林分累积土壤呼吸显著增加了499 g C m(-2),索林的山毛榉林分增加了274 g C m(-2),而其他四个林分的土壤呼吸未受影响。这两个林分土壤呼吸的增加是由于土壤有机质的微生物分解得到改善。在1997年8月至2000年3月期间,测定了10厘米和100厘米深度的穿透雨和渗流水中的DOC浓度和通量。在对照地块中,10厘米深度处的累积DOC输出量在57至95 g C m(-2) 之间,松林分中的速率最高。堆肥处理显著增加了10厘米深度处的累积DOC输出量31至69 g C m(-2),以及100厘米深度处的0.3至6.6 g C m(-2)。1 between the 10- and 100-cm depths acted as significant sinks for DOC,对照地块中100厘米深度处的累积输出量低得多,为3至11 g C m(-2),堆肥地块中为6至16 g C m(-2)。我们的结果表明,向养分贫瘠的森林土壤单次适度施用成熟堆肥对碳向大气和地下水的损失影响很小。 (注:原文中“1 between the 10- and 100-cm depths acted as significant sinks for DOC”表述似乎不完整,可能影响理解,但按照要求未添加解释。)