When designing intensive gardens, one should know not only moisture capacity of the soil
(Lan et al., 2019), but also the microbiological properties
(Hong et al., 2018) and chemical parameters. Knowledge of soil moisture status enables a highly efficient water supply system, delivering water as needed and eliminating wasteful water usage when irrigation is unnecessary (
Balaji and Pandiarajan, 2022). However, research on soil water-holding capacity has primarily been conducted only in annual crops
(Tamiru et al., 2023). The aisles of most gardens are kept under perennial black steam, which leads to soil washing away in the aisles
(Kabelka et al., 2019).
Changes in soil properties are observed in trunk strips. Since apple tree leaf litter is a valuable source of mineral elements
(Chen et al., 2019) and phytostimulators
(Mertoglu et al., 2018), the soils of some orchards are more in content of exchangeable calcium, mobile mineral phosphorus, exchangeable magnesium, absorbed potassium, nitrates
(Lan et al., 2019), organic phosphorus
(Paul et al., 2018) and number of microorganisms compared to forest soils. One of the causes of soil degradation isthe loss of humus and nitrogen Based on the ratio of organic carbon
(Unnikrishnan et al., 2023).
Content and physical clay in soil, it is possible to judge the degree of degradation and potential buffering of the soil. Moreover, in woody communities on clay soils, the reserves of organic carbon and nitrogen due to leaf litter are approximately twice as high as those on sandy soils. As the apple tree grows, the lowest moisture capacity of the soil may change. It is known that, without irrigation, the greatest depth of soil desiccation reaches 160-170 cm when the orchard is 9 to 17 years old. Understanding the moisture reserves in apple orchard soils is mportant when studying orchard mulching
(Neilsen et al., 2003). Moreover, with increasing orchard age, moisture reserves in the soil tend to decrease
(Li et al., 2019). Starting from the 10
th year of the apple tree’s life, moisture reserves in the orchard soil become significantly lower than those in arable soils under field crop rotations and this difference further increases by the orchard’s 19
th year. The most critical aspect of modeling agricultural ecosystems and the environment is the accurate prediction of spatial variability in soil properties
(Rajalakshimi et al., 2025) This is precisely why our article addresses the challenges of soil cover heterogeneity in intensive orchards. A specific fungal microflora is formed in the rhizosphere of the apple tree, which accelerates the destruction of cellulose, inherent in all forest ecosystems. The study of the zone of trunk strips of apple plantations allow us to reveal the mechanism of the effect of apple roots on the soil. Apple tree roots secrete oxalic and malic acids into the soil
(Li et al., 2019). The bacterium Bacillus methylotrophicus CKAM, isolated from the root endosphere of healthy apple trees, produces mainly gluconic and oxalic acids with small amounts of 2-ketogluconic and formic acids
(Mehta et al., 2014). The bacterium Pseudomonas aeruginosa (strain An-15-Mg) is closely associated with roots of apple tree and produces succinic, malonic, citric, malic, chymic, quinic, tartaric, fumaric and lactic acids
(Ranjna et al., 2017). For 35 years of operation of the apple orchard, significant acidification occurred in the 15-45 cm soil layer (
Niedźwiecki, 1991). The granulometric composition of the soil in any fruit growing area is very important for the longevity of apple orchards. On the Loess Plateau of China, which has in light loamy granulometric composition, the cultivation of apple orchards in dry years leads to deep desiccation of the soil by several meters and the danger of wind erosion
(Min et al., 2020). Loamy soils have a richer species composition of soil fungi than sandy loam. On brown clay-alluvial soil, argon chernozem and clay-illuvial chernozem, apple tree plantations are most productive with a physical clay content of 20-40% (
Mãrghitaş et al., 2012). The results indicated that, the rankings of soil health index were generally organic > green > conventional and 95% of the orchards were rated as the grades of moderate (40-60) to better (60-80). Soil health index in green orchards with different cultivation durations followed the pattern of gradual increase over 5 years. The mprovement of soil fertility, soil aggregation structure and soil bio-community were crucial improvement of soil health, prevent soil degradation and promote soil sustainability in this region, particularly under the circumstance of encouraging green agriculture development. In Shanghai (China), a local comprehensive methodology used for assessment soil conditions in gardens with organic, environmentally friendly and traditional farming methods has been successfully developed and applied
(Cao et al., 2023). In horticultural sites, a common method of assessing tillage involves comparing data collected before the garden is established with data gathered after the operation period ends. However, this method does not comply with a fundamental principle of experimental design-the principle of a single variable difference. This principle requires that only one factor varies between the compared conditions to accurately attribute observed changes to that factor alone. Since many environmental factors (
e.
g., climate, soil aging) change over time, this method cannot fully isolate the effect of tillage, limiting the reliability of conclusions. If we compare the data before the garden was laid with the data after it was uprooted, can we reliably say that the changes occurred due to the influence of the garden? After all, during the period of operation of long-term plantings, the soil, in addition to agrotechnical factors, is also influenced by the climate, as a result of which the soil changes even if nothing grows on it. In scientific research, control is used for comparative evaluation, which excludes the effect of the studied factor, but is under equal other conditions. Virgin areas located nearby can be used to assess the level of soil exhaustion in industrial plantations, but this is not always possible. We suggest using the row spacing center of an intensive garden as a control, which is especially important from an agrotechnical point of view. The purpose of our research was to suggest evaluating changes in the soil properties of the apple tree rhizosphere in intensive orchards by comparing them with soil fertility in the middle of the garden aisles.