Forecast basis and method for coal resource forecasting

Coal resources forecast

First, the basis and method of prediction

Coal resource forecasting is one of the main tasks of the third national coalfield forecasting. It is required to comprehensively summarize the achievements in coalfield census and exploration, coalfield geological research since the second coalfield forecast, and a new understanding of the geological conditions of coalfields. Based on the prediction, it may be found that the coal resources are in the storage area and its potential resources and coal and coal quality, pointing out the prospects for the general survey of coal. The basic premise of this coal resource forecast is:

(1) The second coal field prediction (1975 ~ 1980) The basic understanding of the formation and distribution of coalfields in China and the related prediction results are the basis and starting point of this work.

(2) The practical results accumulated in coalfield geological surveys, censuses, explorations and coal mine developments completed since 1976 are the actual materials and basis for improving the degree of geological research in coalfields and carrying out a new round of forecasting.

(3) Since the "Sixth Five-Year Plan" (1981 ~ 1985), especially during the "Seventh Five-Year Plan" and "Eighth Five-Year Plan" period

Completed a number of important regional coalfield geological research topics, including the coal-slip structure and coal-seeking research in eastern China, the Late Paleozoic coal-collecting law and coal-seeking research in North China, and the Late Permian coal-bearing strata sedimentary environment in the eastern Sichuan Research on coal accumulation law, coal accumulation law and coal resource evaluation in Ordos Basin, sedimentary environment and coal accumulation law of Permian coal-bearing strata in South China, relevant provinces (regions) in coal-bearing stratum sedimentary environment, coal accumulation law, coal prospecting prediction The research on evaluation and some new theories and viewpoints in the field of coalfield geology in recent years have laid a theoretical foundation for this coal resource forecast.

(4) The research on the coal resources prospects conducted by the Ministry of Geology and Mineral Resources (1983 ~ 1988) and the relevant results of the China Coal Resources Series (1989 ~ 1992) prepared as a reference.

The coal resource forecast is conducted at the national and provincial (district) levels. The forecasting work of each province (district) is carried out under the unified guidance of the basic ideas, technical routes and working methods of the “Third National Coalfield Forecasting Work Outline”, with coalfields or mining areas as the basic working units, and carried out on larger scale drawings. It is then integrated across the province (region) and is ultimately reflected on the drawings of 1 in 500,000 (1, 1 million in Xinjiang and Inner Mongolia). When the national summary is based on the national, according to the requirements of system, overall and scientific, based on the provincial (regional) forecast data, the statistical results of the provinces (regions) are summarized and compiled, and the distribution map of 1/200,000 Chinese coal resources is compiled. And establish a national coal resource database as part of the national coal resource data information system.

When forecasting coal resources by province (district) and national level, it mainly considers the geological basis of coal-forming and coal-controlling conditions, as well as the practice basis based on census and exploration results.

The geological background of the generation and occurrence of coal resources in China is diverse. The coal-forming conditions and coal-collecting laws of different coal-forming periods and different coal-forming geotectonic units vary greatly, and the characteristics of coal-producing coal vary. Therefore, in the prediction of coal resources, it is necessary to consider the evolution of coal-bearing basins controlled by paleo-tectonics and paleogeographic conditions and the space-time migration law of rich coal belts, as well as the later deformation and transformation of coal measures, that is, structural coal control. The study of coal metamorphism law and the determination of major metamorphism types, as well as the study of coal rock, coal quality and some special properties of sedimentary characteristics and environmental indicators are also important geological basis for coal resource prediction. In short, comprehensive research on coal-bearing construction, coal-stage deformation and coal metamorphism provides a powerful geological basis for coal resource prediction. The chapters in the previous chapter describe the basic aspects of the above aspects.

The practice basis for coal resource forecasting is the existing exploration and development work in the forecast area and its periphery (peripheral or deep). It is a traditional practice of coalfield prediction to infer unknown (predicted zone) from known (exploration and development zones) based on the geological background (based on coal). The application of integrated geophysical and remote sensing geological achievements in the past decade has become an important means to detect the structural form of coal-bearing basins and to discover hidden coal fields, and to provide a more comprehensive prediction basis than the second coal field prediction.

Due to the different geological conditions and resource conditions of each province (district), different methods are adopted according to the actual situation when calculating the predicted coal resource quantity.

(1) The conditions of coal accumulation are good, the stability of coal seam stability is relatively stable, the later stage transformation is weak, the geological structure is simple, the coal-bearing stratum is basically continuous, and the coal resource occurrence area with higher credibility is predicted, and the arithmetic average block segment is adopted. law. The provinces (regions) in the North China Coal-producing Area, Xinjiang in the Northwest Coal-producing Area, and Sichuan, Guizhou, and Yunnan in the South China Coal-producing Area use this method.

(2) The conditions of coal accumulation are generally stable, the coal seam is relatively stable-unstable, the later reform is more intense, the geological structure is medium, the distribution of coal-bearing strata is discontinuous, and the prediction area with poor prediction credibility is added depending on the geological conditions. The reliability correction coefficient is 0.8~0.5. In areas with poor coal accumulation conditions, unstable coal seams and complex geological structures, the correction factor is 0.5 to 0.4. The measurement parameters of the predicted resource amount are extrapolated from the average of the known parameters when the prediction area is adjacent to the surveyed area and the development area; and the new area widely covered by the new world is interpreted and controlled according to ground geophysical exploration. Presumption or inference.

(3) In some provinces (regions) in South China, Southeast Coast, and Central South, there are also direct storage values ​​of reserves/resource abundance parameters (ie, reserves/resources per unit area of ​​coal-bearing strata) The predicted resource amount is calculated by the prediction area and the reliability coefficient.

Forecast resource Q = βxExs

In the formula, the β prediction confidence coefficient (0.8~0.4), the E known area reserve/resource abundance (104t/km2), and the s prediction coal area (km2).

(4) The early Cretaceous basin group in the Erlian coal-bearing area of ​​Inner Mongolia has a low degree of geological work, and the coal-producing parameter information (coal-bearing area and coal-bearing property) is small. The calculation of the predicted resource amount in this area is based on the known Unknown regression analogy mathematical model.

The method firstly analyzes the weights of six factors including the coal-bearing degree controlled by the coal-bearing zone, the structural location, the basin structure type, the thickness of the coal-bearing stratum, the basement depth and the coal seeing in the borehole. Importance), multiplied by the scores corresponding to different classification criteria (1.0, 0.5, 0, respectively, indicating good, medium, and poor), to obtain the single factor coal advantage and the combination of the six factors Coal advantage (x). Take the comprehensive coal-rich favorableness of the known coal-bearing basin with its resource abundance--the coal-bearing rate (y) (104t/km2), and perform the statistical regression calculation after natural logarithm conversion to obtain the regression equation y= ! + bx (13 known areas in the second coal-bearing zone are a = 2.189, b = 5.701). Therefore, the 53 kinds of other coal-producing coal-bearing basins (regions), which are defined by regional adjustment, ground geophysical exploration, and rare control drilling, will be used to calculate the comprehensive coal-consolidation advantage x. The coal content rate y is obtained according to the regression equation y = a / bx. The multiplication value of the coal-bearing area S and the coal-bearing rate y of the coal-bearing basin (district) is predicted to be the predicted resource amount of the prediction area.

Mobile Scissor Lift:

Hydraulic Vertical Aerial Work Platform is made of high quality steel. The Scissor Lift Table is single-phase 220v AC power or three-phase 380v AC power.

Elevating Work Platform control has two ways: manual pump which is equiped for the use in case power is cut off and electric.

Mobile scissor lift heights: ranging from 4m, 6m, 8m, 10m, 12m, 14m.

Mobile Scissor Lift Specification Table:

MODEL

PLATFORM SIZE

(mm)

LIFT CAPACITY

(kg)

LIFT HEIGHT

(m)

OVERALL SIZE

(mm)

WEIGHT

(kg)

SJY0.5-4

2100*830

500

4

2250*950*1100

800

SJY0.5-6

2100*830

500

6

2250*950*1200

880

SJY0.5-7

2100*830

500

6.8

2250*950*1280

970

SJY0.5-8

2100*930

500

8

2250*1060*1380

1050

SJY0.5-9

2100*930

500

9

2250*1060*1500

1165

SJY0.5-10

2100*1230

500

10

2250*1350*1530

1360

SJY0.5-11

2100*1230

500

11

2250*1350*1650

1400

SJY0.5-12

2550*1530

500

12

2796*1670*1750

2260

SJY0.5-14

2812*1530

500

14

3067*1730*1810

2486

SJY0.5-16

2812*1600

500

16

3067*1810*2080

3063

SJY0.5-18

3070*1600

500

18

3321*1810*2080

3900

MODEL

PLATFORM SIZE

(mm)

LIFT CAPACITY

(kg)

LIFT HEIGHT

(m)

OVERALL SIZE

(mm)

WEIGHT

(kg)

SJY1.0-4

2100*1200

1000

4

2250*1350*1180

1250

SJY1.0-6

2100*1200

1000

6

2250*1350*1300

1400

SJY1.0-8

2100*1200

1000

8

2250*1350*1420

1585

SJY1.0-10

2100*1200

1000

10

2250*1350*1530

1700

SJY1.0-12

2550*1530

1000

12

2796*1670*1750

2560

SJY1.0-14

2812*1600

1000

14

3067*1810*1900

3230

MODEL

PLATFORM SIZE

(mm)

LIFT CAPACITY

(kg)

LIFT HEIGHT

(m)

OVERALL SIZE

(mm)

WEIGHT

(kg)

SJY1.5-6

2100*1530

1500

6

2250*1750*1530

1780

SJY1.5-8

2100*1530

1500

8

2250*1750*1690

2070

SJY1.5-10

2100*1530

1500

10

2250*1750*1850

2250

SJY1.5-12

2550*1530

1500

12

2796*1762*1850

2900

SJY1.5-14

2816*1600

1500

14

3045*1852*1960

3400

MODEL

PLATFORM SIZE

(mm)

LIFT CAPACITY

(kg)

LIFT HEIGHT

(m)

OVERALL SIZE

(mm)

WEIGHT

(kg)

SJY2.0-6

2100*1530

2000

6

2250*1750*1530

1780

SJY2.0-8

2100*1530

2000

8

2250*1750*1690

2070

SJY2.0-10

2100*1530

2000

10

2250*1750*1850

2250

SJY2.0-12

2550*1600

2000

12

2796*1852*1954

3200

SJY2.0-14

2816*1600

2000

14

3067*1852*2230

3900

MODEL

PLATFORM SIZE

(mm)

LIFT CAPACITY

(kg)

LIFT HEIGHT

(m)

OVERALL SIZE

(mm)

WEIGHT

(kg)

GTJY05A

1.15×0.7m

240

3

1.3*0.76*1.95

545

GTJY05

1.28×0.7m

240

3

1.44*0.76*1.83

535

GTJY06

1.28×0.7m

240

4

1.44*0.76*1.95

590



Mobile Scissor Lift

Application Area: 

Height Electric Mini Scissor Lift is an equipment used widely in aerial work, such as granary, bus station, railway station, airport. Hydraulic Lift Table can used in gas station and aerial pipeline for the equipments installations and maintenance.


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