Agriculture/3. Arable farming, ground
science and agrochemistry
Candidate of Agricultural Sciences Shilov M.P, 1st
year student Anisimova E.S
RSE "Kostanai State University A.Baitursynov", Kazakhstan
BIOLOGICAL VALUE OF THE
TECHNOLOGIES OF RESTING ON THE SOUTHERN BLACK EARTH OF THE NORTHERN KAZAKHSTAN
Biological diagnostics of new agricultural
methods is essential requirement of conservation cropping
system of the Northern Kazakhstan. At present time
this situation has particular significance with active implementation of resource saving
technologies of crop growing focused on the soil
fertility conservancy.
In connection
with this, the biological diagnostics of different preparation
technologies for complete fallow and cropped fallow were made on the Southern
heavy loamy black earth of the Kostanai region. Complete fallow was preparing
on zonal technology with 5 mechanical processing. In a cropped fallow the oat
mixture with pea was sowed in the second half of summer together with harvest
at the end of September. Determination of soil microorganisms was carried out
by the appropriate methods.
The experiment showed an active influence of
preparation methods the fallow field microbiological regime of the soil (Table
1).
Table 1
Indexes of soil biological activity of complete fallow and
cropped fallow, layer 0-20 cm (average for 2008-2011).
Indexes
|
Complete fallow |
Cropped fallow |
Wheat
fallow
|
|
|
complete |
cropped |
|||
|
The number of microbial
association, million/g of soil; |
57,6 |
31,4 |
33,9 |
43,4 |
|
bacteria: |
|
|
|
|
|
accounting for the millieu MPA, million/g |
12,3 |
10,4 |
9,7 |
10,2 |
|
accounting for the milieu SAA, million/g |
36,7 |
17,3 |
19,4 |
26,8 |
|
Actinomycetes:
accounting for the ÊÀÀ, million/g |
8,2 |
3,5 |
4,6 |
6,1 |
|
Nitrifying, thousand/g |
3,1 |
1,6 |
1,8 |
2,4 |
|
Cellulose-decomposing (bacterias+
actinomycetes), thousand/g |
347,8 |
182,1 |
200,3 |
292,9 |
|
Decaying of soil,% |
59,3 |
35,6 |
33,5 |
38,7 |
In the soil of complete fallow under favorable conditions of temperature, humidity
and aeration develop all types of microbial associations rapidly. Dominating position among them
(78%) took the microorganisms assimilate mineral forms of nitrogen (bacteria
and actinomycetes on milieu SAA). Another common group (21%) are bacteria
that use organic nitrogen (accounting for MPA).
Broad ratio there between is
indicative of intensive crop residues and mineralization of soil organic matter
with the production a large amount of nitrate nitrogen.
The high number of nitrifying
bacteria - 3.1 thousand/g soil indicates on its strong accumulation. The high content of available
forms of nitrogen stimulates intense multiplication of cellulose-decomposing
microorganisms-347,8 thousand/g.
As a result, in the soil of complete fallow there is activity of microorganisms, accompanied with an intense process of mineralization of
plant residues and organic matter. Much tension of microbiological regime is
confirmed by general indicator of soil biological activity - decomposition
linen. Its disintegration within 30 days averaged 59.3%
Seeding of fallow-grown crop has a significant influence on the course of
biological processes. When this happens, in the soil of cropped fallow there is
no rearrangement in the microbial composition and change of the dominant forms.
However, there is a general reduction in all types of quantitative microbial
coenosis. Primarily, the population of microflora consuming mineral nitrogen
reduced in 2.1 times. At the same time the reducing of ammonifying bacteria are
much weaker (16.8%). This leads to a narrowing of the ratio between
microorganisms taken into account on SAA and MPA, and is a sign of attenuation
of active processes of mineralization. As a result of the flow rate of
productive moisture and biological nitrogen fixation of the oat mixture with
pea the number of nitrifying bacteria is reduced to 48.4%. Due to a lack of
available forms of nitrogen the development of cellulolytic microorganisms is
inhibited - 182.1 thousand/ha.
Together, the noted changes reduce the celluloselytic ability of soil.
Decomposition of cellulose is 23.7% (absolute value) is less than complete
fallow and compose 35.6%. In general, the slowing of soil biological activity
in a cropped fallow should be seen as a positive development, conducive to
reducing the rates of organic-matter degradation.
When
the postcuts of the oat mixture with pea enters the soil late in the autumn that does
not significantly
alter the level of biological activity.
It is connected to
the seasonal quantitative decrease of microbial attenuation and its biochemical
activity in this period. Therefore the influence of
accumulated organic mass for microbiological regime appears in spring next
year. However, in the early spring (seed) period biological processes in the
soil of complete fallow flow more active.
Under the cropped fallow the activity of microorganisms is inhibited in a result of the reduced
temperature due to the presence of the oat mixture
with pea postcut on the
surface. The reflection of these differences is the cellulolytic ability of the
soil. In condition of complete fallow the cellulose decomposition degree for 20
days exposure reached 0-10 cm 15,8-22,5 in the layer, at a depth of 10-20cm -
8,8-11,3%. In a cropped fallow the tissue disintegration was less intense -
7,1-10,0 and 12,6-17,4%. During the growing season of
wheat microbiological regime undergoes significant changes. The enter the soil
of allow-grown crop culture organic mass serves as energy propagation material
of all taxonomic groups of microorganisms.
Compared with complete
fallow the total number of microbial
association increased to 28%. The significant changes indicates to the
strengthening of the mineralization processes in the quantitative composition
of bacteria which assimilates mineral nitrogen, nitrifying bacteria and
cellulolytic microbes. As a result, there is a general increase in biogenic
soil, which exhibits in the decomposition rate of cellulose. The cellulose
decay energy was higher in cropped fallow than in
complete fallow - in the layer 0-10 cm 5,6-7,3, at a depth of 10-20 cm - on
3,3-4,4%. The increasing of biological activity all over the depth of arable
layer strengthens the mobilization of available items that improve nutritional
conditions in the initial phases. Thus, the biological basis of the cropped fallow technology
in the steppes is shown with
the help of describing studies. The seeding of fallow-grown crop relieve tensions
microbiological processes and reducing the amount of organic-matter degradation
in a fallow period. Receipt of plant residues the
oat mixture with pea mixture increases the biological activity of the soil under the first
wheat.