CELLULOSOLYTIC ACTIVITY OF SOILS OF THE ODESA CITY

S. Domuschy, V. Trigub
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Abstract

Problem Statement and Purpose. Cellulose cleavage is of great importance in the carbon cycle, as it contains more than 50% of all organic carbon in the biosphere. This is a fairly stable organic compound that is destroyed only by very strong oxidants. Under natural conditions, the destruction of cellulose is carried out by various microorganisms that produce cellulase enzymes. The activation of cellulose decomposition is influenced by temperature, pH level, soil aeration, biological properties of vegetation, etc. Being very resistant to physicochemical factors, cellulose is easily decomposed by microorganisms with the release of carbon, which in the form of various compounds is involved in creating soil fertility. Cellulose is broken down by aerobic microorganisms (bacteria and fungi) and anaerobic mesophilic and thermophilic bacteria. The peculiarity of cellulose-destroying microorganisms is their high demand for nitrogen sources. Soil-destroying soil microorganisms are the most important suppliers of organic matter to various groups of microorganisms (including nitrogen-fixing) in the common food chain. Since the activity of cellulose-destroying microorganisms also depends on the presence of available phosphorus and other elements in the soil, the degree of decomposition of fiber can be considered to reflect the direction of microbiological processes in general. Cellulolytic activity indicates the intensity of biological processes in the soil. The more intensively the cellulose decomposes, the faster the biological cycle of elements takes place and the fuller the plants are provided with nutrients. Therefore, cellulose activity is used as one of the indicators of biological activity of the soil environment. Data &Methods. The author, in the study of cellulosolytic activity of soils in the city of Odessa, used the method of applications (laying in the soil strips of filter paper or linen cloth fixed on the glass). Applications were laid vertically in the upper 15-cm layer of soil of 5 pieces on the site. A month later, they were dug up, carefully washed from the soil and decay products, dried and weighed again. Cellulolytic activity was determined by weight loss of exposed tissue. Results. As a result of research on the study of cellulolytic activity of soils in the city of Odessa, it was found that cellulolytic activity is an important indicator of the intensity of destructive processes in the soil. The intensity of cellulose decomposition in the soil is determined by the combined action of several factors: weather conditions, the nature of vegetation, the amount of organic matter entering the soil, soil type, its physical properties, chemical composition. In an urban environment, the intensity of cellulosolytic processes is also regulated by the nature and degree of anthropogenic impact on soil, atmosphere and vegetation. The intensity of cellulose destruction in the city soils is estimated to be very weak, weak and medium. The cellulolytic processes in the soils of the city of Odessa in 2021 were stimulated by abundant precipitation (r = 1,000). The decrease in CA in some parts of the city may be due to minimal anthropogenic impact on the soil cover.
敖德萨市土壤纤维素水解活性研究
问题陈述和目的。纤维素裂解在碳循环中具有重要意义,因为它含有生物圈中50%以上的有机碳。这是一种相当稳定的有机化合物,只有很强的氧化剂才能破坏它。在自然条件下,纤维素的破坏是由产生纤维素酶的各种微生物进行的。纤维素分解的激活受温度、pH值、土壤通气性、植被生物特性等因素的影响。纤维素对物理化学因素有很强的抵抗力,很容易被微生物分解并释放出碳,碳以各种化合物的形式参与土壤肥力的产生。纤维素被好氧微生物(细菌和真菌)和厌氧嗜中温和嗜热细菌分解。纤维素破坏微生物的特点是它们对氮源的高需求。破坏土壤的土壤微生物是共同食物链中各种微生物(包括固氮微生物)最重要的有机物供应者。由于破坏纤维素的微生物的活性也取决于土壤中有效磷和其他元素的存在,纤维的分解程度可以被认为反映了微生物过程的总体方向。纤维素分解活性表明土壤中生物过程的强度。纤维素分解得越剧烈,元素的生物循环就进行得越快,植物得到的营养就越充分。因此,纤维素活性被用作土壤环境生物活性的指标之一。数据的方法。作者在敖德萨市土壤纤维素水解活性的研究中,采用了应用的方法(在土壤中铺设固定在玻璃上的滤纸或亚麻布条)。应用程序垂直铺设在现场5块15厘米的土壤上层。一个月后,它们被挖出来,小心地从土壤和腐烂物中洗掉,晾干并再次称重。纤维素水解活性通过暴露组织的失重来测定。通过对敖德萨市土壤纤维素分解活性的研究,发现纤维素分解活性是土壤中破坏过程强度的重要指标。纤维素在土壤中分解的强度是由几个因素的共同作用决定的:天气条件、植被的性质、进入土壤的有机质的数量、土壤类型、其物理性质、化学成分。在城市环境中,纤维素水解过程的强度也受到人为对土壤、大气和植被影响的性质和程度的调节。纤维素在城市土壤中的破坏强度估计为极弱、弱和中等。丰富的降水(r = 1000)刺激了2021年敖德萨市土壤中的纤维素分解过程。城市某些地区CA的减少可能是由于对土壤覆盖的人为影响很小。
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