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首页> 外文期刊>Frontiers in Environmental Science >Urbanization Leads to Increases in pH, Carbonate, and Soil Organic Matter Stocks of Arable Soils of Kumasi, Ghana (West Africa)
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Urbanization Leads to Increases in pH, Carbonate, and Soil Organic Matter Stocks of Arable Soils of Kumasi, Ghana (West Africa)

机译:城市化导致加纳库马西(西非)可耕土壤的pH值,碳酸盐和土壤有机质增加

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Tropical soils typically have low cation exchange capacity and nutrient contents. Both are enhanced by soil organic matter (SOM), which is thus particularly important for the fertility of these soils. In this study, we assessed the influence of urbanization on SOM, carbonate contents and pH of arable soils of Kumasi (Ghana, West Africa), since rapid urban sprawl is widespread in West Africa, whereby in many West African cities urban farming is pivotal to the food security of their population. Based on satellite imagery for the year 1986, we distinguished long-term and short-term urban arable soils, whereby long-term urban soils were urban already in 1986 (thus ? 30 years, as soil sampling took place in 2016), and short-term urban soils became urban afterwards (< 30 years). We took 618 undisturbed topsoil samples (0-10 cm) from 206 urban arable fields. The factors land-use (maize fields) and soil (Ferric Acrisols) were kept largely constant. The fine-earth was analysed for pH (water), carbonate contents, loss on ignition (LOI), total C (TC) and N (TN). SOM contents were obtained from LOI (SOMLOI). All element contents were transformed to bulk soil element stocks per m2. Differences between short-term and long-term urban soils were identified by a set of linear mixed models. Coarse fragments were more abundant in the long-term (16%) compared to the short-term (10%) urban soils, because of solid municipal waste that accumulates over time in urban soils. TC and SOMLOI concentrations of the fine earth, pH and C/N ratios were all significantly higher in the long-term urban soils. SOC concentrations in the fine earth, as well as bulk soil stocks of TC, SOC and SOMLOI were also higher in the long-term urban soils, but at a lower degree of confidence, due to variable bulk densities and contents of coarse fragments. We conclude that dumping of organic and inorganic waste (including ash, bones, egg shells, concrete and mortar) increases SOM stocks and soil pH, but also leads to accumulation of non-degradable solid materials (including plastic, metals etc.). These findings point to the need of an improved urban waste management system, separating degradable and non-degradable waste.
机译:热带土壤通常具有较低的阳离子交换能力和营养成分。两者均通过土壤有机质(SOM)增强,因此对于这些土壤的肥力特别重要。在这项研究中,我们评估了城市化对库马西(西非加纳)可耕土壤的SOM,碳酸盐含量和pH值的影响,因为快速的城市扩张在西非十分普遍,因此在许多西非城市中,城市农业对于他们人口的粮食安全。根据1986年的卫星图像,我们区分了长期和短期的城市耕作土壤,其中长期的城市土壤已经在1986年成为城市(因此,在30年,因为2016年进行了土壤采样),而短期长期城市土壤随后(<30年)变为城市土壤。我们从206个城市耕地中采集了618个未扰动的表土(0-10厘米)样本。土地利用(玉米田)和土壤(铁粉刺)的因素基本保持不变。分析了细土的pH(水),碳酸盐含量,烧失量(LOI),总碳(TC)和氮(TN)。 SOM内容来自LOI(SOMLOI)。将所有元素含量转换为每平方米的散装土壤元素储量。短期和长期城市土壤之间的差异通过一组线性混合模型确定。与城市的短期(10%)相比,长期(16%)的粗粒碎片更为丰富,这是因为随着时间的推移,城市土壤中会积聚固体废物。在长期城市土壤中,细土的TC和SOMLOI浓度,pH和C / N比均显着较高。在长期的城市土壤中,细土中的SOC浓度以及TC,SOC和SOMLOI的散装土壤储量也较高,但由于散装密度和粗粒含量的变化,置信度较低。我们得出的结论是,有机和无机废物(包括灰烬,骨头,蛋壳,混凝土和灰浆)的倾倒会增加SOM库存和土壤pH值,但也会导致不可降解的固体物质(包括塑料,金属等)的积累。这些发现表明,有必要改进城市废物管理系统,将可降解和不可降解废物分开。

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