ÓÄÊ   662.271.575.15 (045)

 Abdurahimov X.A-dotsent

Kholkhujaev B-student TIIM

 

 

Physical and chemical properties of soil, destruction by explosion energy and the development of  basic principles of remediation on
their recovery

Physico-chemical properties of soil and contaminated land is not charged by the energy of the explosion, the main principles of remediation to restore the destroyed on of soils.

Building collapses reclamation, particularly earthworks, ponds, dams, embankments channels, collectors and others, performed by two fundamentally different methods-diggers and using the energy of the explosion. These methods have been around for decades, but the comparitional damage assessment of the environment and to restore damaged ecosystems was performed. With fine views of nature protection measures both methods have positive and negative effects.

When used earthmoving machinery construction project is saturated by heavy machinery and a lot of manpower. Long terms earthen buildings severely contaminate the surrounding area with oil products, litter it unusable parts, accessories and waste. Violated the composition, structure of the soil, the top layer of contaminated ponds and woodlands. The explosive way, depending on the volume of earthworks 2-8 times faster construction than using machinery. The share of used machinery and labor are significantly reduced. During explosive method, there are side effects on virtually all components of the ecosystem effects of an explosion are particularly vulnerable to soil components.

Issues related to the loss of soil fertility, have hardly been studied, due to the disposal of its fertile upper horizon of the action of the explosion energy, and this type of pollution is distributed over long distances.
Known effect of an explosion on an area of
​​1.5x1.5 on the chemical composition of the soil, which is an increase of oxides of nitrogen in the soil at 0.02-0.03 mEq, but without changing the pH = 7.2, and the effect of residual products of the explosion on the environment.

We developed the basic principles of remediation work on the restoration of damaged soil under the effect of the explosion energy on the basis of chemical analysis. The chemical composition of the soil is necessary for a proper understanding of the quantitative distribution of chemical cations and anions, which come into contact other chemicals. In light of the above areas surveyed construction of irrigation canals and reservoirs of Bukhara and Navoi region and the Republic of Karakalpakstan. In this field used standard experimental techniques with the sampling of the soil and subsoil. In view of further remediation developed a special scheme of samples of soils and soils. Theessence of this scheme are as follows:

1. Samples from different channel elements.
2. At different distances from brust vern to the border of the channel of distribution of separate clumps of soil and gruhntum mass.
3. Soil sampling on the arable sector.


Inspection of the area where the explosion was carried out showed that in the 1.5 km x 1.0 km soil-ground surface is covered with a layer of dust, which can thicken with the approach to Nabal breed.
Inspection of the area where the explosion was carried out showed that in the1.5km x1.0kmsoil-groundsurface is covered with a layer of dust, which can thicken with the approach to Nabal breed.Samples were selected from the study area before and after the explosion, made ​​the chemical analysis

of the soil(Table)

 

A comparative analysis of the results tables set increase of oxidized nitro gen in the soil, almost 0.02-0.03mEqsoil. However, the pH value of 7.2has changed. Probably, there was an instantaneous interaction of nitrogen oxides with the minerals of the so, therefore apparent equivalence pH before and after an explosion. In the samples of soil taken from the surface of Nabal, Zaphod-sated increase of nitric oxide, which increases with decreasing fraction of 0.02 to 35.25 mg / kg. It should be noted the very low humus content of the soil mass after the explosion - 0.09-1.32%, whereas for the comparison of the arable horizon it reached 2.8%. Because of the specific features of the location of these soils in their natural ¬ Venn addition of high humus content is at an average depth of 15 cm, as the top layer is frequently updated by the insertion of fresh sand. Soils with a depth of 30-40 cm  beans differ same degree of salinity, which is usually clearly seen in the first half.

 


 ¹

 Test, earth and grounds

Content,% 

 pH

Content mg-ekv/ 100g earth 

 humus

humidity 

Anions

cations

 HCO-1

CL -

SO 42-

NO 3-

∑ 

 Ca2+

Mg 2+

Na +

∑ 

 1

 Navoi canal- bottom

0,28

4,19

6,6

0,2

0,44

15,60

0,02

16,26

14,97

0,65

0,70

16,32

 2

 Medium-side

0,19

9,44

6,6

0,2

0,39

15,30

0,01

15,90

14,65

0,64

0,76

15,95

 3

 Travel horizon old canal

3,66

6,20

7,0

0,31

1,47

16,46

0,03

18,27

14,43

1,51

2,82

18,76

 4

 Medium side

1,47

3,66

7,0

0,26

2,85

11,36

0,13

14,60

9,15

2,16

3,52

14,83

 5

 Trevel horizont collector “chinka”

1,66

0,86

7,6

0,26

2,26

3,55

0,07

6,14

2,80

1,08

2,40

6,28

 6

 Bottom

3,43

3,43

7,9

0,27

81,48

19,20

0,02

100,97

5,12

25,04

70,88

101,04

 7

 Ceiling partion

2,92

3,11

8,2

0,27

115,82

33,96

0,09

150,14

12,40

42,00

92,85

147,25

 1*

 Navoi canal-

 bottom

0,18

4,47

6,4

0,24

0,44

15,19

0,05

16,32

14,97

0,65

0,70

16,32

 2*

 Medium-side

0,09

9,40

6,4

0,24

0,39

15,29

0,03

15,95

14,65

0,54

0,76

15,95

 3*

 Travel horizon old canal

2,76

6,16

6,8

0,34

1,47

16,45

0,70

18,96

14,43

1,51

2,82

18,76

 4*

 Medium side

0,47

3,63

6,8

0,29

2,85

11,36

0,32

14,82

9,15

2,15

2,52

14,82

 5*

 Trevel horizont collector “chinka”

0,60

1,83

7,4

0,29

2,26

3,55

0,19

6,29

2,80

1,08

2,41

6,29

 6*

 Bottom

0,81

3,41

7,7

0,29

81,47

19,21

0,07

101,04

5,12

25,04

70,88

101,04

 7*

 Ceiling partion

1,32

3,09

8,0

0,29

115,82

33,95

0,19

150,25

12,39

42,01

92,85

147,25

Ïîäïèñü: Physico-chemical properties of soi l and contaminated land in the place melioration objects


 

Salts of calcium sulphates predominate compared with11 nitrates, carbonates and chlorides. When comparing the nitrate content(Table I)is easily seen to increase them after the explosion .Analysis of the aqueous extracts of the soil allows us to consider them neutral or slightly alkaline environment. Gray-brown soils are extremely low capacity of absorption of water (1.83-9.40%), due to low content of humustion. 80-90% of the cations are Ca2 + ions, 10 -20%-Mg2 +. Particular attention should be paid to the anionic composition of the soil and rocks ground, Is observed SO42-concentration to 33.95meq/100g soil, Cl-, to115.82mg-
ekv/100g,which in turn harms the development of remediation, in such cases for the removal of the soil before plant in necessary decontaminate on of the area.

Results of analyzes and discussion of physical and chemical properties of soils formed the basis for the formulation of the basic principles ¬ types of remediation measures for the restoration of damaged soil structure under the influence of the energy of the explosion. The essence of these principles ¬ types are as follows:
1. Accounting for soil and genetic characteristics of disturbed soil and thrown to the surface by the action of the explosion energy ground rocks and soils. In this case, optionally ¬ necessary to install a complex of factors operating at the initial stages of soil formation, to identify the main determining the differentiation of the profile at different stages, to track their progress.
2. Use of landscape-geochemical characteristics of the area to assess the migration of salts and soil-ground layer on the reclaimed areas;

3. Consideration of regional differences. One of the key indicators, taking into account the necessary remediation work, - the salt content in soils is ejected to the surface during blasting operations.
      Work should be carried out in stages. The first stage - reclamation and preparation aimed at improving the physical and biological properties, nutrient status and stratification of rocks. At this stage, a lot of attention paid to the selection of cultures that best meets the soil conditions. The main forms of life, grow well in the soil studied rocks are perennial long vegetating plants.

      The second phase - the development of soil reclamation plants    by plants resistant against deep salinity and excess nitrate salts on the soil surface. At this stage of work should pay attention to agromeliorative study aimed recovered but trees and shrubs of groves.

      Thus, we studied the physicochemical properties of uncontaminated soil and contaminated land under the influence of the explosion energy, the main principles of remediation for the restoration of damaged soils.

 

                                           

 

USED LITERATURE

1.     Áåéìèíñîí Ì. Å.,  Êîð÷åâñêèé Â. Ô.,  Ìóðàòîâà Ì. Õ. Õóñàíõîäæàåâ Ì.Ã.,  Òàäæèáàåâ Ñ.Ì.  Ãèäðîòåõíè÷åñêîå ñòðîèòåëüñòâî. 1991. ¹ 3.  Ñ. 21-23.

2.     Þ.Ä.ÍÎÐÎÂ, Õ.À.ÀÁÄÓÐÀÕÈÌÎÂ, Â.Ð. ÐÀÈÌÆÎÍÎÂ, À.Ñ.ÒÓÐÀÅÂ. Óçáåêñêèé õèìè÷åñêèé æóðíàë. 2002. ¹ 3. Ñ. 42-46.