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Long term impact of organic amendments on forest soil properties under semiarid Mediterranean climatic conditions

机译:半干旱地中海气候条件下有机改造对森林土壤性质的长期影响

摘要

Soil degradation affects more than 52 million ha of land in countries of the European Union (Hueso-Gonzálezet al., 2016). This problema is particularly serious in Mediterranean areas, where the effects of anthropogenicactivities (tillage on slopes, deforestation, and pasture production) add to problems caused by prolonged periodsof drought and intense and irregular rainfall (Martínez-Murillo et al., 2016). Depending on the scale of study,soil organic carbón (SOC) dynamics in Mediterranean forests have been found to be particularly sensitive tofactors related to seasonal changes in temperature and soil moisture (Casals et al., 2000; Eaton et al., 2008;Hueso-González et al., 2014). During dry periods in theMediterranean area, the lack of water entering the soilmatrix reduces organic contributions to the soil (Parras-Alcántara et al., 2016). These processes lead to reducedsoil fertility and soil loss (García-Orenes et al., 2010). Restoring the native vegetation is one of the most effectiveways to control soil degradation in Mediterranean areas, especially in very degraded areas. In the initial monthsafter afforestation, vegetation cover establishment and soil quality could be better sustained if the soil wasamended with an external extra source of organic matter (Hueso-González et al., 2016).The goal of this study was to test the effect of various organic amendments on select soil properties over a54-month period. Five amendments were applied in an experimental set of plots: straw mulching (SM), mulchwith chipped branches of Aleppo Pine (Pinus halepensis L.; PM), sheep manure compost (SH), hydroabsorbentpolymers (HP) and sewage sludge (RU). Plots were afforested following the same spatial pattern, and amendmentswere mixed with the soil at the rate 10Mg ha-1.Soil from the afforested plots was sampled in the following: (i) spring 2012 (6 months postafforestation);(ii) spring 2013(18 months postafforestation); (iii) spring 2014 (30 months postafforestation); (iv) spring 2015(42 months postafforestation) and; (v) spring 2016 (54 months postafforestation). The sampling strategy for eachplot involved the collection of four disturbed soil samples taken from the surface (0 to 10-cm depth). The soilproperties analyzed were as follows: (i) soil organic carbon (SOC); (ii) pH; (iii) electrical conductivity (EC); (iv)aggregates stability (AS) and; (v) texture (TE).Regarding to soil aggregate stability, 54 month after the afforestation, the percentage of stable aggregateshas increased slightly in all the treatments (HP, RU, PM, SM and SH) in relation to control. Specifically, thedifferences were recorded in the fraction of macroaggregates ( 0.250 mm). The largest increases have beenassociated with SM, PM and RU treatments. Although the SM, PM and RU treatments helped to maintain the SOCat high levels in the 54 months following application. Conversely, not significant differences relative to the controlplots were found for the pH, EC or texture, 54 months following afforestation. To conclude, these results showedan increase in the SOC and the stability of the macroaggregates when soil is amended with sludge, pinus mulchand straw much. This fact has been due to an increase in the number cementing agents due to: (i) the applicationof pinus, straw and sludge had resulted in the release of carbohydrates to the soil; and thus (ii) it has favored thedevelopment of a protective vegetation cover, which has increased the number of roots in the soil and the organiccontribution to it.
机译:在欧盟国家中,土壤退化影响了超过5200万公顷的土地(Hueso-Gonzálezet等,2016)。这个问题在地中海地区尤为严重,那里的人为活动(耕种对斜坡,森林砍伐和牧场生产)的影响加剧了长期干旱,强降雨和不规则降雨引起的问题(Martínez-Murilloet al。,2016)。根据研究规模,发现地中海森林中土壤有机碳(SOC)的动态变化对与温度和土壤湿度的季节性变化有关的因素特别敏感(Casals等,2000; Eaton等,2008; Hueso -González等人,2014年)。在地中海地区的干旱时期,缺少水分进入土壤基质减少了有机物对土壤的贡献(Parras-Alcántara等,2016)。这些过程导致土壤肥力降低和土壤流失(García-Orenes等,2010)。恢复原生植被是控制地中海地区尤其是极度退化地区土壤退化的最有效方法之一。在植树造林后的最初几个月中,如果用外部额外的有机物质对土壤进行改建,则植被覆盖的建立和土壤质量将得到更好的维持(Hueso-González等人,2016)。在54个月的时间内对选定的土壤特性进行了各种有机改良。在一组试验性地块上进行了五项修正:秸秆覆盖(SM),阿勒颇松(Pinus halepensis L .; PM)覆盖有碎枝的覆盖,羊粪堆肥(SH),吸水性聚合物(HP)和污水污泥(RU)。按照相同的空间格局对绿地进行绿化,并以10Mg ha-1的速率将改良剂与土壤混合。对绿化地的土壤取样如下:(i)2012年春季(造林后6个月);(ii)2013年春季(造林后18个月); (iii)2014年春季(造林后30个月); (iv)2015年春季(造林后42个月);以及(v)2016年春季(造林后54个月)。每个图的采样策略涉及从地表(0至10厘米深度)采集四个扰动的土壤样本。分析的土壤性质如下:(i)土壤有机碳(SOC); (ii)pH; (iii)电导率(EC); (iv)汇总稳定性(AS);以及(v)质地(TE)。关于土壤团聚体的稳定性,在造林后54个月,与对照相比,所有处理(HP,RU,PM,SM和SH)中稳定团聚体的百分比略有增加。具体地,差异记录在大骨料的分数(0.250mm)中。增幅最大的是SM,PM和RU处理。尽管SM,PM和RU处理有助于在施用后的54个月内将SOC维持在高水平。相反,造林后54个月,pH,EC或质地与对照图没有显着差异。综上所述,这些结果表明,当土壤被污泥,松树秸秆大量改良时,土壤有机碳的增加和大型骨料的稳定性。这是由于以下原因导致胶结剂数量增加的原因:(i)施用松树,稻草和污泥已导致向土壤中释放碳水化合物;因此(ii)它有利于保护性植被的发展,这增加了土壤中根的数量和对土壤的有机贡献。

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