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首页> 外文期刊>Forest Ecology and Management >Impact of compaction on two sensitive forest soils in Lorraine (France) assessed by the changes occurring in the perched water table
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Impact of compaction on two sensitive forest soils in Lorraine (France) assessed by the changes occurring in the perched water table

机译:栖息下水桌中发生变化评估洛林(法国)两种敏感森林土壤的影响

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The mechanisation of forestry operations is too recent in France to have enough perspective and scientific knowledge of the effects on extensively managed soils. Two experimental sites on soils sensitive to compaction (silty acidic soils laying on top of a clayey subsoil) were set in Lorraine (France). A gentle and controlled compaction of these physically very analogous soils was carried out during spring 2007 at the Azerailles site (AZ) and during spring 2008 at the Clermont-en-Argonne site (CA). Immediate changes were observed for all ecosystem physical, chemical and biological functioning indicators. Soil restoration dynamics were followed using continuous monitoring of numerous parameters, including soil moisture and occurrence of a perched water table (PWT) (monitored at a daily time step) and PWT chemistry (monthly time step). Mid-term monitoring (7-8 years) results showed that both soils shifted towards a hydromorphic soil type attested by the increase in PWT frequency and duration, which invaded the soil upper layers, leading to characteristic Fe, Mn and S mobility and a change in organic compounds stability. Though soil types were very similar, the PWT characteristics varied notably between both sites. The mean residence time of the PWT was shown to be a major driver of its geochemistry, but with strong interaction with soil characteristics. A previous study made on both sites suggested that soil clay content and clay mineralogy controls the PWT dynamics through effects on aggregation. From a PWT perspective, seven years of monitoring were insufficient to observe any soil compaction recovery in the richer soil of AZ but a partial recovery was observed for the chemically poorer soil (CA). Compaction durably impacted the two studied soils and the probability that a new compaction event may occur before the complete recovery from the first disturbance must be considered in forest management.
机译:林业运营的机械化太近期,在法国近来,有足够的视角和科学知识对广泛管理土壤的影响。在洛林(法国)设定了对压实敏感土壤的两种实验遗迹(粘土上铺设在粘土上的粉质酸性土壤)。在2007年春天的Azerailles位点(AZ)和2008年春天的康涅狄克因位点(CA),在2007年春季进行了温和的和受控压实。针对所有生态系统的物理,化学和生物功能指标观察到立即改变。遵循土壤恢复动力学,采用连续监测许多参数,包括土壤水分和栖息的水位(PWT)(在每日时间步骤监测)和PWT化学(月度时间步长)。中期监测(7-8岁)结果表明,两种土壤都朝向潮湿频率和持续时间增加的潮湿土壤类型转移,这侵入了土壤上层,导致特有的Fe,Mn和S流动性和变化在有机化合物稳定性。虽然土壤类型非常相似,但PWT特性在两个位点之间均值变化。 PWT的平均停留时间被证明是其地球化学的主要驾驶员,但具有强烈的土壤特征的互动。在两个网站上进行的先前研究表明,土壤粘土含量和粘土矿物通过对聚集的影响控制了PWT动态。从PWT的角度来看,七年的监测不足以观察AZ的富裕土壤中的任何土壤压实恢复,而是针对化学较差的土壤(CA)观察到部分恢复。压实持久影响了两种研究的土壤,并且在森林管理中必须考虑在森林管理中完全恢复之前发生的新压实事件的可能性。

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