The south-eastern slope of the Greater Caucasus The impact of micromobiements to the micromiological process and fermentativ activity on territorial lands

Research Article | DOI: https://doi.org/10.58489/2836-3590/003

The south-eastern slope of the Greater Caucasus The impact of micromobiements to the micromiological process and fermentativ activity on territorial lands

  • V.T.Mammadzade

Institute Of Soil Science and Agro Chemistry of Anas-Baku-2019

*Corresponding Author: V.T.Mammadzade

Citation: V.T.Mammadzade, (2022). The south-eastern slope of the Greater Caucasus the impact of micromobiements to the micromiological process and fermentativ activity on territorial lands. Journal of Pollution and Effects on Community Health. 1(1). DOI: 10.58489/2836-3590/003.

Copyright: © 2022 V.T. Mammadzade,, this is an open access article distributed under the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.

Received: 04 November 2022 | Accepted: 21 November 2022 | Published: 18 December 2022

Keywords: hydrothermic conditions, fertilizers, complex fertilizers (NAFK-90), bacteria, radical mushrooms and fungi, microorganisms, light, heat, food, cobalt, zinc and manganese.

Abstract

in 2012-2017, the activity of bacteria, ray fungi and microscopic fungi from microorganisms was studied in field experiments with the aim of studying the effect of micronutrients on the productivity of winter wheat in moderately eroded gray mountain-brown soils. The regularity of the activity of the microorganisms that play a major role during the vegetation period of wheat was studied. It was found that the micronutrients given to the soil increased the activity of groups of microorganisms in all variants of the experiment. Thus, the effect of micronutrients on the activity of bacteria was greater. Likewise, micronutrients also increased the activity of fungi and fungi. has increased. The activity of bacteria and fungi has increased. Also, does this group of microorganisms develop better, especially in conditions without humidity? From these 5-6 years of research carried out by us, we can draw the conclusion that microelements significantly revive the microbiological process in eroded soils, as a result of which decomposition and synthesis of decay in the soil is significantly improved, and the process of humus formation is accelerated.

Introduction

figure 1

As it is known, the problem of industrial production in the country is a matter of anger as an important issue, the problem of efficient use of land and food production. The lands of the mountainous area are considered a large source of source in the increase in agricultural products in Azerbaijan.

 In general, you need to take complex zonal combat measures against erosion to use soil lands in the mountainous areas. This explains that the erosion process is widespread in connection with the proper conduct of economic work in a complex geomorphological environment.

For many years, the soil has been washed as a result of the erosion process, productivity deteriorates and the volume of nutrients is reduced sharply and their motivation is very limited.

The first turn of the bruises in the falling soils, the total number of microorganisms is a significant amount of 1G.

In the variant of the ink fertilizer (NAFK-90) (NAFK-90) (NAFK-90), this increase was 750-4071 thousand.

The maximum increase in the number of microorganisms was in the options provided by cobalt, zinc and manganese.

Development of microorganisms (bacteria, radical and fungi) is accelerating when hydrotmite conditions are improved in June-July and expand the volume of fertilizers.

The total number of microorganisms in the variants in the variants in June increased by 229-4861 thousand.

In the variant of the complex fertilizer, the total number of microorganisms in June was 631 to 185 thousand in June. The rapid development is to provide the population with enough food.

Due to the demand of the day, as a demand for the development of grain production for the purpose of the current economic crisis, state support is in the center of this area.

Reduced, its fraction composition deteriorates and decreases the moving part of agronomically valuable humin acids. Thus, the erosion process has a negative impact on the basic parameters of the humus process in the lands.

The erosion process also weakens the intensity of all biochemical, fermentative processes and lands from carbon dioxide (CO2).

The erosion process is also very weak in the microbiological process.

The soil microfa was a solution to biochemical processes, especially in the regulating human synthesis and mineralization, which regulates these processes.

Research has been found in the result of erosion process, water-physical, agrochemical characteristics and nutrients. As a result, the productivity of agricultural crops decreases. This has a negative impact on the biological productivity of our planet.

Taking into account the damage caused by erosion into the blessing of the soil, the application of agro-technical measures increasing ink alarm in the fight against it is a great need.

The application of a fertilizer system is very important in these events.

In the last 30 years, the republic's fertilizer employees surrendered in the background of simple, complex mineral fertilizers and the republic in the erosion lands of the republic.

Previous savings in this issue

In other parts of the Tong Union, sufficient materials were collected.

 However, the physiological and biochemical bases of mineral fertilizers under the country's erosion lands were not well studied.

This article, presented to the discussion of the readers, was dedicated to the "influence of micronutinals" and its settlement. Here, in the south-eastern part of research facilities, fall wheat, complex mineral fertilizers and complex fertilizers and complex fertilizers in the south-eastern part of autumn wheat are dedicated to the results of physiological research and biochemical grounds

I. The impact of micromelements in the micromology

Progress and analysis of materials:

As can be seen from the desktop figures, in April, the microbiological process (in early April) is not intensively. However, despite this, the microbiological process has increased a variable variant of a certain amount of fertilizer.

The use of microelements was more than the activities of microorganisms with the choices of cobalt, manganese and zinc.

In this case, this study, the impact of fertilizers in this study, it was possible to see this table. In general, the complex zone management measures should be re-performed and important T erosion in order to effective use Land, Especially Land in Mountainous Areas.

This is Explained by The Fact That The Process of Erosion is Widespread Due To The Proper Management of Economic Activities in A Complex Geomorphological Environment Rosion

Enough Materials Were Also Collected in Other Regions of the Tong Union. However, The Physiological And Biochemical Bases Of Individual Species of Mineral Fertilizers Under Cereals in The Country Were Not Well-Studied.

This article, which is presented to the readers' discussion, is Dedicated to the notxue of "The Impact of Micronutinals in the Micromemiological Process" and ITS Solution. Here, in the Southern-Eastern Part of the Arearch Facilities, in the South-Eastern part of the Back of WHEAT, Complex Mineral Fertilizers and Complex Fertilizers and Complex Fertilizers Are Dedicated To The Study of Physiological and biochemical bases

I. Micromelements of The impact to the Microbiological Process

Progress and Analysis of Materials:

As Can Be Seen From The Figures of The Table, in April, The Microbiological Process (in Early April) is not fully intensively. However, in Spite Of This, The Microbiological Process Increased to A Certain Amount Of Fertilizer Versefully Verangers.

The Total Number of Microeliuts in The Field of Practice has increased by 337-4861 Thousand in 1G of the Total Number of Microorganisms.

In The Variant Of The Complex Fertilizer (NAFK-90) in The Fertless Variante (NAFK-90), This Inrease WAS 750-4071 Thousand.

The maximum increase in the number of microorganisms Was in the Options Provided by Cobalt, Zinc and Manganese.

The Development Of Microorganisms (Bacteria, Radical and Fungi) is accelerated When Hydrothermic Conditions Are Improved in June-July And Expanding The Scope of Ferilizers.

The Total Number Of Microelganisms in The Veritts Relative to The Research is Determined in June, increased by 229-4861 Thousand in the Soil.

In The Variant of The Complex Fertilizer, The Inrease in The Number of Microorganisms Relative to A Fertile Variant Has Changed Between 631 and 185 Thousand in June.

The Use of Microelements Was More Than The Activity Of Microorganisms With Options Applied to Cobalt, Manganese and Zinc.

In This Study, This Study, The impact of Fertilizers in This Study in July, IT WAS Possible To See The Following Table.

Table.1.The impact of microelements to the microbiological process on the ground (0-30 cm, 1g in the soil)

 

Variants of practice

 

2012

April

 

June

 

July

Bacteria

 

Shui Mushrooms

 

Mushrooms

 

Microong. total number

 

Bacteria

 

Shui Mushrooms

 

Mushrooms

 

Microong. total number

 

Bacteria

 

Shui Mushrooms

 

Mushrooms

 

Microong. total number

 

Control (no fertilizer)

9782

998

24

10804

9883

1020

24

10927

9309

1030

8

10347

NAFK-90 (background)

13801

1046

28

14875

11229

1057

27

12303

10819

1067

11

11897

Fon+3kq/ha Ni

14346

1167

33

15546

13694

1178

29

14801

11649

1188

12

12749

Fon+3kq/ha Zn

15125

1202

36

16360

14124

1223

34

15381

12088

1234

20

13342

Fon+3kq/ha Cu

14536

1002

34

15569

11687

1023

27

12737

8565

1044

6

9615

Fon+3kq/ha B

14484

1055

30

15569

14264

1066

32

15362

11727

1140

13

12880

Fon+3kq/ha Co

15451

1362

39

16852

16437

1384

51

17879

14613

1427

41

16081

Fon+3kq/ha Mn

14500

1205

37

15742

15037

1227

42

16306

12806

1259

17

14082

                                                                                           Table. 1's name 

 

Variants of practice

2013

April

                                         

June

July

Bacteria

 

Shui Mushrooms

 

Mushrooms

 

Microong. total number

 

Bacteria

 

Shui Mushrooms

 

Mushrooms

 

Microong. total number

 

Bacteria

 

Shui Mushrooms

 

Mushrooms

 

Microong. total number

 

Control (no fertilizer)

10750

878

18

11646

10845

900

20

11765

1045

882

41

11868

NAFK-90 (background)

11440

964

23

12277

11440

986

23

12449

11531

981

44

12556

Fon+3kq/ha Ni

11450

986

24

12460

11528

997

25

12550

18036

987

49

19072

Fon+3kq/ha Zn

12100

1025

27

13152

13018

1043

29

14090

17426

1073

50

18549

Fon+3kq/ha Cu

18940

963

23

11926

10971

963

24

11958

15052

949

36

16037

Fon+3kq/ha B

11560

1048

33

12654

11654

1059

38

12751

16780

1044

62

17886

Fon+3kq/ha Co

13720

1065

37

14822

14640

1065

40

15745

18412

1062

69

19543

Fon+3kq/ha Mn

10630

1015

30

11875

11071

1026

34

12131

17044

1019

55

18063

Table. 1's name

 

Variants of practice

 

2014

April

June

July

Bacteria

 

Shui Mushrooms

 

Mushrooms

 

Microong. total number

 

Bacteria

 

Shui Mushrooms

 

Mushrooms

 

Microong. total number

 

Bacteria

 

Shui Mushrooms

 

Mushrooms

 

Microong. total number

 

Control (no fertilizer)

6256

826

56

7138

7116

946

78

8140

6528

968

71

7567

NAFK-90 (background)

7581

882

70

8533

8061

991

116

0168

7843

1002

108

8845

Fon+3kq/ha Ni

7914

971

132

9017

8406

1001

168

9575

8034

1015

155

9204

Fon+3kq/ha Zn

8884

962

111

9957

9463

1028

140

10491

9190

1039

127

10356

Fon+3kq/ha Cu

6532

872

71

7475

7088

922

83

8163

6892

1003

81

7976

Fon+3kq/ha B

7785

829

96

8780

8223

1019

126

9363

8004

1030

115

9149

Fon+3kq/ha Co

9868

1019

142

11029

10032

1052

186

11270

9824

1063

164

11051

Fon+3kq/ha Mn

8759

944

109

9812

9429

1042

135

10588

9242

1053

128

10423

Table. 1's name

 

Variants of practice

 

2015

April

 

June

 

July

Bacteria

 

Shui Mushrooms

 

Mushrooms

 

Microong. total number

 

Bacteria

 

Shui Mushrooms

 

Mushrooms

 

Microong. total number

 

Bacteria

 

Shui Mushrooms

 

Mushrooms

 

Microong. total number

 

Control (no fertilizer)

4369

750

35

5154

4739

760

80

5579

4478

815

51

5344

NAFK-90 (background)

5059

803

42

5904

5439

825

116

6380

5081

870

62

6013

Fon+3kq/ha Ni

6134

890

46

7070

6199

912

121

7232

6156

923

64

7143

Fon+3kq/ha Zn

7331

870

50

8251

7917

921

212

9050

7483

954

87

8524

Fon+3kq/ha Cu

5162

790

37

5989

5802

813

200

6815

5206

878

51

6135

Fon+3kq/ha B

6721

860

62

7643

6971

871

135

7977

6753

904

84

7741

Fon+3kq/ha Co

9498

915

105

10508

9716

936

216

10868

9575

980

108

10663

Fon+3kq/ha Mn

9074

849

92

10015

9422

860

204

10486

9204

947

86

10237

                                                                                                        Table. 1's name

 

Variants of practice

2016

April

June

July

Bacteria

 

Shui Mushrooms

 

Mushrooms

 

Microong. total number

 

Bacteria

 

Shui Mushrooms

 

Mushrooms

 

Microong. total number

 

Bacteria

 

Shui Mushrooms

 

Mushrooms

 

Microong. total number

 

Control (No Fertilizer)

2457

865

68

3390

5517

752

81

6350

5056

572

35

5663

NAFK-90(background)

3190

923

125

4238

5585

816

101

6502

5513

818

69

6392

Fon+3kq/ha Ni

3620

958

144

4722

5612

927

106

6645

5152

1035

57

6244

Fon+3kq/ha Zn

3800

1006

147

4953

6457

784

140

7381

5806

871

68

6745

Fon+3kq/ha Cu

2653

891

73

3617

6291

869

128

7288

6057

798

102

9657

Fon+3kq/ha B

3412

944

129

4485

6431

957

186

7574

5981

866

86

6533

Fon+3kq/ha Co

4113

1025

160

5298

6539

985

174

7698

6053

981

75

7109

Fon+3kq/ha Mn

3304

970

142

4416

6609

920

197

7726

6355

1264

97

7716

As can be seen from the analysis of the figures in the table, in July, the total number of microorganisms in 1 g of soil increased by 1582-8675 thousand in the options with micronutrients compared to the option without fertilizer.

As can be seen from the figures in the table, the total number of microorganisms in 1 g of soil increased from 666 to 1550 thousand compared to the version without fertilizer.

II. Effect of trace elements on enzymatic activity in eroded soils

The great importance of the enzymatic processes in the soil is explained by their active participation in biochemical processes and humus formation. He also noted that the formation and transformation of substances in the soil takes place with the direct participation of enzymes.

As is known, the activity of enzymes is related to many soil ecological factors. In addition to biotic factors, abiotic factors affect the intensity of the enzymatic process. So, in eroded soils that have lost their fertility, biological and biochemical processes stop, which leads to weakening of the enzymatic process.

The effect of trace elements on the enzymatic process was studied in moderately eroded steppe brown soils developed in the territory of the research object. The study was conducted in the experimental field planted under the wheat plant in April, May, June and July.

As can be seen from the figures in table 2 below, in April, catalase activity was 7.0-13.0 cm3 in 1 minute in the non-fertilized variant, while it was 8.6-17.4 cm3 in the variants with compound fertilizer. The highest activity of catalase was observed in variants given zinc, cobalt and manganese.

 According to research years, the activity of catalase in June varied between 5.5-15.3 cm3 in the variant without fertilizer, 8.7-16.0 cm3 in the variant given complex fertilizer, and 9.0-25.4 cm3 in the variants given micronutrients. Thus, compared to the variant without fertilizer, the activity of catalase was 1.1-9.5 cm3 in the variant with complex fertilizer, and 3.1-13.1 cm3 in the variant with trace elements. In general, trace elements significantly increased the activity of catalase, as a result of which the biochemical processes in eroded soils were significantly improved.

As it is known, enzymes are secreted by the vital activity of soil microorganisms, the root system of plants and mesofauna, and their role in nature and the biosphere is multifaceted.

Enzymes, as biological catalysts, speed up chemical processes in the body a hundred thousand times.

Catalase breaks down the hydrogen compounds accumulated in the soil into water and oxygen molecules. Considering all this, it can be shown that the effect of trace elements on the enzymatic process is very important.

Table 2. Effect of trace elements on the biological activity of eroded soils

Variants of practice

Depth,              cm

  CO2 mg/kg/h

2012

2013

2014

2015

2016

April

 

June

 

july

April

 

June

 

july

April

 

June

 

july

April

 

June

 

july

April

 

June

 

july

ControlNo Fertilizer)

0-30

49.5

73.3

40.4

42.2

44.0

46.0

44.0

44.0

18.3

30.8

40.3

37.5

24.2

30.8

36.7

NAFK-90(background)

-“-

62.3

78.8

47.7

49.5

49.4

53.2

55.0

56.0

20.0

37.0

51.3

50.6

33.0

44.0

49.5

Fon+3kq/ha Ni

-”-

64.2

80.7

55.0

50.1

50.1

51.4

59.0

61.5

23.3

52.8

64.2

59.6

39.5

46.5

50.7

Fon+3kq/ha Zn

-”-

67.9

93.5

67.8

47.7

53.2

58.7

60.5

63.8

23.3

60.9

69.7

65.8

70.4

72.5

73.2

Fon+3kq/ha Cu

-“-

66.0

91.6

51.3

44.0

46.0

42.2

56.8

59.4

21.6

39.6

53.2

50.6

28.5

33.0

49.5

Fon+3kq/ha B

-“-

77.0

100.9

64.2

53.2

57.5

57.0

68.0

68.2

30.8

60.4

66.0

65.8

37.4

50.6

60.0

Fon+3kq/haCo

-“-

88.0

130.2

84.3

67.2

69.7

73.3

69.7

70.5

45.8

66.0

84.4

74.8

72.5

74.8

75.2

Fon+3kq/ha Mn

 

84.3

119.2

73.3

47.3

66.0

71.3

66.0

66.0

29.1

60.8

68.0

66.0

61.2

63.8

70.1

Table 3. Effect of trace elements on enzymatic activity in eroded soils

Variants of practice

Depth,              cm

Catalase cm3 O2 g/min

2012

2013

2014

2015

2016

April

 

June

 

july

April

 

June

 

july

April

 

June

 

july

April

 

June

 

july

April

 

June

 

july

Control (No Fertilizer)

0-30

8

15,0

5.7

9.6

11.6

15.3

7.8

7.5

5.0 

13.0

13.7

13.2

8.1

15.3

19.4

NAFK-90(background)

-”-

11,2

16,0

7.0

11.5

13.4

24.8

8.0

8.7

7.0

14.1

14.7

14.3

10.0

17.5

21.5

Fon+3kq/ha Ni

-“-

12,1

17,1

10.0

15.0

16.8

22.6

8.6

9.0

7.2

15.0

15.6

15.2

10.4

19.6

22.3

Fon+3kq/ha Zn

-”-

12,3

18,6

10.7

18.5

18.8

25.8

9.1

10.0

7.0

16.4

17.6

16.9

11.2

21.5

24.8

Fon+3kq/ha Cu

-“-

12,4

16,9

8.8

17.2

13.5

20.6

7.5

7.9

6.0

14.4

14.9

14.9

9.9

16.2

21.8

Fon+3kq/ha B

-”-

12,6

20.5

9.1

16.0

17.2

21.1

8.8

9.2

7.8

15.6

16.7

16.0

10.6

20.8

23.8

Fon+3kq/ha Co

-“-

13,5

23.4

12.2

19.4

19.9

28.4

9.6

10.4

8.7

17.4

18.7

18.0

12.0

25.5

26.0

Fon+3kq/ha Mn

 

13,0

22.7

9.8

17.4

18.0

27.8

6.7

8.7

7.9

16.3

17.5

17.0

10.3

24.0

25.0

Table 4. Effect of trace elements on the activity of nitroreductase enzyme in eroded soils (0-30 cm layer)

Variants of practice

Depth,              cm

to the activity of the nitroreductase enzyme in mg/kg body weight in 24 hours (for the last 3-year research period)

2014

2015

2016

April

 

June

 

july

April

 

June

 

july

April

 

June

 

july

Control (No Fertilizer)

0-30

39,0

43.2

45.0

35.0

46.0

43.6

42.5

41.5

37.5

NAFK-90(background)

-”-

31.1

42.9

43.2

27.5

45.5

52.5

25.0

31.5

35.0

Fon+3kq/ha Ni

-“-

31.1

41.7

46.3

27.5

41.8

47.5

35.0

40.0

35.5

Fon+3kq/ha Zn

-”-

26.0

43.0

43.3

34.5

45.5

53.0

32.5

40.0

38.0

Fon+3kq/ha Cu

-“-

32.4

42.7

42.5

27.5

47.5

53.0

22.5

47.5

40.0

Fon+3kq/ha B

-”-

28.5

43.1

43.6

34.5

47.5

53.5

25.0

47.5

42.5

Fon+3kq/ha Co

-“-

23.3

42.5

43.6

32.5

47.5

57.5

25.0

40.5

40.0

Fon+3kq/ha Mn

 

23.3

42.1

43.6

32.5

46.8

52.5

30.0

45.5

42.0

Table 3 shows the activity of the nitroreductase enzyme. As can be seen from this figure, the activity of nitrate reductase in all variants after fertilization in early spring was lower than the non-fertilization variant. Thus, in the variant without fertilizer, the activity of nitrate reductase was 35.0-39 mg/kg in April, while in the variant with compound fertilizer it was 27.5-31.1 mg/kg. Nitrate reductase activity decreased by 7.5-7.9 mg in the variant with complex fertilizer compared to the variant without fertilizer.

In April, the activity of nitrate reductase was 23.3-32.4 mg/kg in 24 hours in the variants applied microelements, which decreased by 2.6-15.7 mg/kg compared to the variant without fertilizers. 

Nitrate reductase activity was significantly reduced in variants where zinc, cobalt and manganese were applied. In July, the activity of nitrate reductase increased sharply. Thus, its activity (in 24 hours) is 43.2-42.5 mg/kg in the variant without fertilizer, 43.2-52.5 mg/kg in the variant with complex fertilizer, and 42.5-57.5 mg in the variant with micronutrients. /kg has been.

Among microelements zinc, cobalt and copper significantly increased the activity intensity of nitrate reductase.

As can be seen from the figures in the table, the effect of micronutrients on the activity of nitrate reductase was not observed in April, and its activity was lower in the experimental variants than in the variant without fertilizer. 

In this regard, it should be noted that the nitrate reductase enzyme ensures the conversion of nitrates into nitrites in the soil.The effect of trace elements on the activity of urease enzyme was also studied in the last 3-year research period in Arizia. 

It was determined that trace elements significantly increase the activity of urease. June-July) is higher than in spring (April). 

Thus, in April, the amount of urease in the version without fertilizer was 0.33-0.69 mg (NH3 in 24 hours) in 1 g of soil, while it was 0.84-1.02 mg in the version with compound fertilizer. 

Nickel, zinc and urease activity was higher in variants given cobalt. In July, the activity of urease was 0.68-1.14 mg in the variant without fertilizer, 1.02-1.33 mg in the variant with complex fertilizer, and 0.74-1.98 mg in the variant with micronutrients. The activity of urease was high in June (1.40-2.09 mg) and July (0.80-2.09 mg). In general, the options providing nickel, zinc and cobalt were effective regardless of hydrothermal conditions.

Table 5. The impact of microelemenes to the activity of the ureasa enzyme in the ingredient land (in 0-30 cm)

Variants of practice

Depth,              cm

to the activity of nitroreductase enzyme mg/kg body weight in 24 hours (for the last 3-year research period

2014

2015

2016

aprel

iyun

iyul

aprel

iyun

iyul

aprel

iyun

iyul

Control (No Fertilizer)

0-30

0.33

0.80

0.68

0.69

1.40

1.14

1.15

1.44

1.68

NAFK-90(background)

-”-

0.84

1.24

1.02

1.02

1.47

1.33

1.39

1.88

1.99

Fon+3kq/ha Ni

-“-

1.18

1.65

1.36

1.15

1.85

1.55

1.44

2.26

2.35

Fon+3kq/ha Zn

-”-

1.50

1.78

1.49

1.24

1.88

1.57

1.61

2.33

2.39

Fon+3kq/ha Cu

-“-

0.38

0.87

0.74

0.90

1.58

1.27

1.32

1.74

1.78

Fon+3kq/ha B

-”-

0.46

0.93

0.88

1.10

1.51

1.31

1.52

2.02

2.12

Fon+3kq/ha Co

-“-

1.57

2.09

1.73

1.37

2.09

1.98

1.74

2.46

2.66

Fon+3kq/ha Mn

“-

0.87

1.27

1.15

1.10

1.75

1.72

1.54

2.19

2.26

Currently, as a result of the widespread use of nitrate-containing fertilizers in agriculture, nitrates accumulate in the soil, which has a great role in environmental pollution. 

Nitrates accumulated in the soil are also collected in agricultural plants and transferred to human and animal bodies and cause various pathological conditions. In such conditions, the nitrate reductase enzyme is of great importance. Nitrate reductase serves human health and nature protection by breaking down nitrates accumulated in the soil

            As can be seen from the analysis of the figures in the table, in July, the total number of microorganisms in 1 g of soil increased by 1582-8675 thousand in the options with micronutrients compared to the option without fertilizer.

As can be seen from the figures in the table, the total number of microorganisms in 1 g of soil increased from 666 to 1550 thousand compared to the version without fertilizer.

CONCLUSION

1. Microelements increased the activity of groups of microorganisms in all variants. The effect of microelements on the activity of bacteria was greater.

2. Microelements also increased the activity of ray fungi and fungi. The activity of bacteria and fungi increased. This group of microorganisms develops especially well in conditions without humidity.

3. From the conducted 5-year research, it can be concluded that microelements significantly revive the microbiological process in eroded soils, as a result of which decomposition and synthesis of decay in the soil is significantly improved, and the process of humus formation is accelerated.

References