Рис. 6. Пространственная изменчивос

Рис. 6. Пространственная изменчивость RLQ-осей

На рисунках, которые отражают пространственную изменчивость осей RLQ-осей 1 и 2 характерными являются области с высокими и низкими значениями осей, которые имеют неправильно-овальную (амебоидную) форму. Анализ данных, представленных ранее, указывает на то, что пространственные паттерны, индицируемые вариабельностью оси 1, в наибольшей степени связаны с неоднородностью почвенных условий в пределах изученного полигона, так как маркером этой оси является твердость почвы в пределах всего почвенного профиля, в пределах которого проведены измерения. Вероятно, именно с этим связана большая контрастность и извитость границ структурных пятен соответствующего пространственного паттерна. Ось 2 также маркируется твердостью, но другим важным маркером является высота травостоя. Можно предположить, что в случае оси 2, твердость почвы является уже не причиной вариабельности экологических условий, а следствием пространственной организации растительного покрова. Известно, что растительность является существенным модулятором ряда почвенных свойств, в том числе и твердости почвы. Таким образом, мы можем заключить, что RLQ-ось 1, отражающая связь почвенных условий и экологических свойств животного населения, обусловлена педогенными факторами. В свою очередь, RLQ-ось 2 отражает организующую роль фитогенных факторов, которые в своем действии на почвенную мезофауну также преломляются через трансформацию почвенных условий.

Результаты (английский) 1:

Figure. 6. Spatial variability of RLQ-axesThe figures, which reflect the spatial variability of the axis 1 and axis RLQ-2 typical are areas with high and low values of the axes that have wrong-oval (ameboidnuû) form. Analysis of the data presented earlier indicate that spatial patterns, variability, 1 axis indiciruemye most closely associated with the heterogeneity of soil conditions within the polygon, studied as a marker of that axis is the soil hardness throughout the soil profile, within which the measured. It is probably related to this is a great contrast and tortuous structural boundaries corresponding spots spatial pattern. Axle 2 also marked firmness, but another important marker is the height of the grass. It can be assumed that in the case of axis 2, the hardness of the soil is no longer a cause of variability of environmental conditions as a consequence of the spatial organization of plant cover. It is known that vegetation is a significant modulator of a series of soil properties and soil hardness. Thus, we can conclude that the RLQ-1 axis, showing the relationship of soil conditions and environmental properties of animal populations, is caused by pedogennymi factors. In turn, RLQ-2 axis reflects the convening role of phytogenic factors which in its effects on soil mezofaunu also refracted through the transformation of soil conditions.

Результаты (английский) 2:

Fig. 6. Spatial variability RLQ-axes of

the figures, which reflect the spatial variability of axes RLQ-axes 1 and 2 are characteristic of the area with the highest and lowest values of the axes, which are irregularly oval (amoeboid) form. The analysis presented above data indicates that the spatial patterns, the displayed variability axis 1, mostly related to the inhomogeneity of the soil conditions in the range studied polygon as a marker of this axis is soil hardness within the whole soil profile, within which carried measurement. Perhaps it is connected with this great contrast and structural boundaries crimp spots corresponding to the spatial pattern. Axis 2 is also marked by hardness, but another important marker is the height of the grass. We can assume that in the case of axis 2, the hardness of the soil is no longer a cause of variability of environmental conditions, as a consequence of the spatial organization of vegetation. It is known that vegetation is essential modulator series of soil properties, including hardness and soil. Thus, we can conclude that the RLQ-axis 1, reflecting the relationship of soil conditions and environmental properties of the animal population, due to pedogenic factors. In turn, RLQ 2-axis reflects the organizational role phytogenic factors in their effect on soil mesofauna also refracted through the transformation of soil conditions.

Результаты (английский) 3:

figure 1. 6. the spatial variability of RLQ - axesin the figures, which reflect the spatial variability of RLQ - axes 1 and 2 are the areas with high and low values of axles, which are wrong овальную (амебоидную) form. analysis of the data reported previously, indicate that the spatial patterns of affinity вариабельностью axis 1, most closely related to the heterogeneity of soil conditions within the изученного polygon, as a marker of this axis is the hardness of the soil throughout the soil profile, within which the measured. possibly, this is a big contrast and извитость limits the spatial pattern of structural patterns. figure 2 also marked the hardness, but another important marker is the height of травостоя. we assume that in the case of the axis 2, the hardness of the soil is not the cause of вариабельности environmental conditions, and the effect of the spatial organization of vegetation. know that vegetation is a significant modulator of several soil properties, including soil hardness. thus, we can conclude that the RLQ axle 1, reflecting the relationship of soil conditions and environmental characteristics of the animal population, due to the педогенными factors. in turn, RLQ - axis 2 reflects the convening role of фитогенных factors which, in its action on the почвенную мезофауну also actually break up the light through the transformation of soil conditions.