Geçiş İklimi Koşulları Altında Farklı Akarsu Yataklarında Yer Alan Toprakların Verimlilik Özellikleri

Bahadır Atmaca
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Abstract

This study was conducted to identify and evaluate some of the fertility characteristics of soils in stream beds in Şebinkarahisar district of the Giresun province of Türkiye, which has a transitional climate between semi-arid and humid climate zones. To this end, a total of 48 soil samples, surface (0-30 cm) and subsurface (30-60/61/62/65 cm), were collected from 24 different sampling points on various stream beds. The textures of the surface and subsurface soils taken were determined as CL, SL, SCL, L, C, and LS. pH values of surface soils ranged from 5.84 to 7.98, and the pH values of subsurface soils ranged from 6.06 to 8.05. Lime contents of the soils without salinity problem ranged from 0.00% to 38.30% for surface soils, and from 0.00% to 37.90% for subsurface soils. Organic matter contents varied between 0.32% and 4.16% for surface soils, and between 0.14% and 2.16% for subsurface soils. While the soils were poor in total nitrogen, phosphorus, zinc and manganese, it was determined that the calcium and copper contents were at sufficient levels. Although deficiencies were detected in some soils for potassium, magnesium and iron, they were generally determined to be at sufficient levels. To deal with deficiencies of macro and micro plant nutrients, including deficiency of organic matter, a fertilization planning is recommended that includes barnyard manure, poultry manure, green manure, compost, vermicompost, and various organic fertilizers containing macro and micro elements. Within the scope of the research, climate classifications were also made according to Thornthwaite, De Martonne-Gottman and Erinç methods by had used 48 years (1965-2012) climate data of Şebinkarahisar district. Plant species and varieties to be grown in the study area should be selected from among those suitable to the transitional climate conditions prevailing in the region. It will also be useful to analyze the stream waters in the areas where soil sampling is done.
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过渡气候条件下不同河床土壤的肥力特征
蒂尔基耶吉雷松省Şebinkarahisar 地区的气候介于半干旱气候和湿润气候之间,本研究旨在确定和评估该地区河床土壤的一些肥力特征。为此,研究人员从不同河床上的 24 个不同取样点采集了地表(0-30 厘米)和地下(30-60/61/62/65 厘米)共 48 个土壤样本。地表土壤的 pH 值介于 5.84 至 7.98 之间,地下土壤的 pH 值介于 6.06 至 8.05 之间。没有盐渍化问题的土壤中,表层土壤的石灰含量在 0.00% 到 38.30% 之间,地下土壤的石灰含量在 0.00% 到 37.90% 之间。表层土壤的有机质含量在 0.32% 至 4.16% 之间,地下土壤的有机质含量在 0.14% 至 2.16% 之间。虽然土壤中总氮、磷、锌和锰的含量较低,但钙和铜的含量达到了足够的水平。虽然在一些土壤中发现了钾、镁和铁的缺乏,但总体上确定它们处于充足水平。为了解决植物宏量和微量营养元素缺乏的问题,包括有机物质缺乏的问题,建议制定施肥计划,包括施用厩肥、禽畜粪便、绿肥、堆肥、蛭石肥料以及含有宏量和微量元素的各种有机肥料。在研究范围内,还根据 Thornthwaite、De Martonne-Gottman 和 Erinç 方法,利用舍宾卡拉希萨尔地区 48 年(1965-2012 年)的气候数据进行了气候分类。应从适合该地区过渡性气候条件的植物品种中选择适合该地区种植的植物品种。对土壤取样地区的溪水进行分析也很有帮助。
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