CN111931374A - Typhoon area landslide stability evaluation method - Google Patents

Typhoon area landslide stability evaluation method Download PDF

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CN111931374A
CN111931374A CN202010799455.XA CN202010799455A CN111931374A CN 111931374 A CN111931374 A CN 111931374A CN 202010799455 A CN202010799455 A CN 202010799455A CN 111931374 A CN111931374 A CN 111931374A
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闫金凯
王文沛
李海龙
刘凯
王志辉
任天翔
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Chinese Academy of Geological Sciences
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Abstract

The invention discloses a landslide stability evaluation method in a typhoon area, which comprises the steps of acquiring each parameter of landslide safety coefficient calculation by collecting geological survey reports or by means of investigation and test; acquiring typhoon level, wind direction, rain intensity and duration parameters according to meteorological information of a typhoon area; calculating a safety factor FS influenced by the property of the slope body according to the acquired parameters1Safety factor FS influenced by rainfall2And safety factor FS affected by wind load3(ii) a And calculating the landslide safety coefficient of the typhoon area according to the obtained safety coefficients, and evaluating the landslide stability of the typhoon area by using the obtained landslide safety coefficient. According to the method, the influence of the typhoon load is considered in the safety coefficient calculation of the typhoon area landslide, so that the stability evaluation of the typhoon area landslide is more practical, and the practicability is improved.

Description

Typhoon area landslide stability evaluation method
Technical Field
The invention relates to the technical field of landslide stability research, in particular to a landslide stability evaluation method in a typhoon area.
Background
At present, typhoon landing is carried out for multiple times every year in coastal areas, typhoon rainstorm induces a large amount of geological disasters, most slopes in the influence range are simultaneously acted by typhoon loads and rainstorm after the typhoon landing, and the typhoon wind level generally reaches dozens of levels, so that the wind load is a non-negligible factor of landslide. The vegetation is luxuriant in the southeast coastal region, and wind load acts on the vegetation, can exert the effect to the vegetation, and this power can be transmitted to the slope body through the vegetation, leads to the stress state of landslide to change to influence the stability of landslide.
In the prior art, the calculation of the landslide safety coefficient in the typhoon area only considers the influence of rainstorm and does not consider the influence of typhoon load on landslide, the evaluation of the typhoon rainstorm type landslide is generally processed according to the common rainfall type landslide, and the landslide safety coefficient considering the wind load action has no scientific and reasonable solution.
Disclosure of Invention
The invention aims to provide a typhoon area landslide stability evaluation method, which considers the influence of typhoon load in the safety coefficient calculation of the typhoon area landslide, so that the stability evaluation of the typhoon area landslide is more practical, and the practicability is improved.
The purpose of the invention is realized by the following technical scheme:
a method for evaluating stability of landslide in a typhoon area comprises the following steps:
step 1, acquiring each parameter of landslide safety coefficient calculation by collecting geological survey reports or by means of investigation and test;
step 2, acquiring typhoon level, wind direction, rain intensity and duration parameters according to meteorological information of the typhoon area;
step 3, calculating a safety factor FS influenced by the property of the slope body according to the parameters obtained in the step 1 and the step 21Safety factor FS influenced by rainfall2And safety factor FS affected by wind load3
And 4, calculating the landslide safety coefficients of the typhoon area according to the safety coefficients obtained in the step 3, and evaluating the landslide stability of the typhoon area by using the obtained landslide safety coefficients.
According to the technical scheme provided by the invention, the influence of typhoon load is considered in the safety coefficient calculation of the typhoon area landslide by the method, so that the stability evaluation of the typhoon area landslide is more practical, and the practicability is improved.
Drawings
In order to more clearly illustrate the technical solutions of the embodiments of the present invention, the drawings needed to be used in the description of the embodiments are briefly introduced below, and it is obvious that the drawings in the following description are only some embodiments of the present invention, and it is obvious for those skilled in the art to obtain other drawings based on the drawings without creative efforts.
Fig. 1 is a schematic flow chart of a method for evaluating stability of a landslide in a typhoon area according to an embodiment of the present invention;
fig. 2 is a schematic sectional view of a model used for calculating the landslide safety coefficient of the typhoon area according to the embodiment of the invention.
Detailed Description
The technical solutions in the embodiments of the present invention are clearly and completely described below with reference to the drawings in the embodiments of the present invention, and it is obvious that the described embodiments are only a part of the embodiments of the present invention, and not all embodiments. All other embodiments, which can be derived by a person skilled in the art from the embodiments of the present invention without making any creative effort, shall fall within the protection scope of the present invention.
The following will describe an embodiment of the present invention in further detail with reference to the accompanying drawings, and as shown in fig. 1, a schematic flow chart of a method for evaluating landslide stability in a typhoon area provided by the embodiment of the present invention is shown, where the method includes:
step 1, acquiring each parameter of landslide safety coefficient calculation by collecting geological survey reports or by means of investigation and test;
step 2, acquiring typhoon level, wind direction, rain intensity and duration parameters according to meteorological information of the typhoon area;
step 3, calculating a safety factor FS influenced by the property of the slope body according to the parameters obtained in the step 1 and the step 21Safety factor FS influenced by rainfall2And safety factor FS affected by wind load3
In this step, as shown in fig. 2, a schematic cross-sectional view of a model adopted for calculating a landslide safety factor of a typhoon area according to an embodiment of the present invention is shown, and with reference to fig. 2:
safety factor FS influenced by slope body property1Obtained by the following formula:
Figure BDA0002626857770000021
wherein, FS1The safety factor is influenced by the property of the slope body;
Figure BDA0002626857770000022
is the internal friction angle of the soil body; alpha is the gradient; c is soil mass cohesion; gamma raysIs the volume weight of the soil body; z is the vertical thickness of the soil layer;
safety factor FS influenced by rainfall2Obtained by the following formula:
Figure BDA0002626857770000031
wherein psi0(Z) is stable matric potential distribution which corresponds to the stable seepage condition of the slope under the initial water content calculated under the condition of not considering rainfall; gamma raywIs the volume weight of water; gamma raysIs the volume weight of the soil body; i isZThe intensity of rainfall is used; kZIs the vertical saturation permeability coefficient; r (t)*) As a function of matric potential response; t is t*Calculating time for normalization; t is*Is the standardized rainfall time.
In a specific implementation, the matric potential response function R (t)*) Obtained by the following formula:
Figure BDA0002626857770000032
Figure BDA0002626857770000033
Figure BDA0002626857770000034
wherein t is time; d0The maximum matrix potential diffusion capacity of the soil; alpha is a slope angle (alpha is more than or equal to 0 and less than or equal to 90 degrees); t is the duration of the rainfall.
Factor of safety FS influenced by wind load3Obtained by the following formula:
Figure BDA0002626857770000035
wherein v is the wind speed; d is the maximum width of the crown; l is the crown height; n is the number of trees on the slope body in unit area; beta is the included angle between the wind direction and the slope direction.
And 4, calculating the landslide safety coefficients of the typhoon area according to the safety coefficients obtained in the step 3, and evaluating the landslide stability of the typhoon area by using the obtained landslide safety coefficients.
In this step, the landslide safety factor of the typhoon zone is influenced by the safety factor FS affected by the properties of the slope body1Safety factor FS influenced by rainfall2And safety factor FS affected by wind load3The composition is obtained by the following formula:
FS=FS1+FS2+FS3
it is noted that those skilled in the art will recognize that embodiments of the present invention are not described in detail herein.
In conclusion, the method provided by the embodiment of the invention considers the influence of the typhoon load in the safety coefficient calculation of the typhoon area landslide, so that the stability evaluation of the typhoon area landslide is more practical, and the practicability is improved.
The above description is only for the preferred embodiment of the present invention, but the scope of the present invention is not limited thereto, and any changes or substitutions that can be easily conceived by those skilled in the art within the technical scope of the present invention are included in the scope of the present invention. Therefore, the protection scope of the present invention shall be subject to the protection scope of the claims.

Claims (4)

1. A method for evaluating landslide stability in a typhoon area is characterized by comprising the following steps:
step 1, acquiring each parameter of landslide safety coefficient calculation by collecting geological survey reports or by means of investigation and test;
step 2, acquiring typhoon level, wind direction, rain intensity and duration parameters according to meteorological information of the typhoon area;
step 3, calculating a safety factor FS influenced by the property of the slope body according to the parameters obtained in the step 1 and the step 21Safety factor FS influenced by rainfall2And safety factor FS affected by wind load3
And 4, calculating the landslide safety coefficients of the typhoon area according to the safety coefficients obtained in the step 3, and evaluating the landslide stability of the typhoon area by using the obtained landslide safety coefficients.
2. The typhoon area landslide stability evaluation method according to claim 1, wherein in step 3, a safety factor FS affected by the property of the slope body1Obtained by the following formula:
Figure FDA0002626857760000011
wherein, FS1Is the nature of the slopeThe safety factor of the influence;
Figure FDA0002626857760000012
is the internal friction angle of the soil body; alpha is the gradient; c is soil mass cohesion; gamma raysIs the volume weight of the soil body; z is the vertical thickness of the soil layer;
safety factor FS influenced by rainfall2Obtained by the following formula:
Figure FDA0002626857760000013
wherein psi0(Z) is stable matric potential distribution which corresponds to the stable seepage condition of the slope under the initial water content calculated under the condition of not considering rainfall; gamma raywIs the volume weight of water; gamma raysIs the volume weight of the soil body; i isZThe intensity of rainfall is used; kZIs the vertical saturation permeability coefficient; r (t)*) As a function of matric potential response; t is t*Calculating time for normalization; t is*The standardized rainfall time;
factor of safety FS influenced by wind load3Obtained by the following formula:
Figure FDA0002626857760000014
wherein v is the wind speed; d is the maximum width of the crown; l is the crown height; n is the number of trees on the slope body in unit area; beta is the included angle between the wind direction and the slope direction.
3. The typhoon area landslide stability evaluation method according to claim 2, wherein the matric potential response function R (t)*) Obtained by the following formula:
Figure FDA0002626857760000021
Figure FDA0002626857760000022
Figure FDA0002626857760000023
wherein t is time; d0The maximum matrix potential diffusion capacity of the soil; alpha is a slope angle; t is the duration of the rainfall.
4. The typhoon area landslide stability evaluation method according to claim 1, wherein in step 4, the landslide safety factor of the typhoon area is a safety factor FS affected by the property of the slope body1Safety factor FS influenced by rainfall2And safety factor FS affected by wind load3The composition is obtained by the following formula:
FS=FS1+FS2+FS3
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CN112733069A (en) * 2021-01-13 2021-04-30 中国地质科学院 Typhoon area bamboo forest landslide safety coefficient calculation method
WO2022033601A1 (en) * 2020-08-11 2022-02-17 中国地质科学院 Typhoon area landslide stability evaluation method

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WO2022033601A1 (en) * 2020-08-11 2022-02-17 中国地质科学院 Typhoon area landslide stability evaluation method
CN112733069A (en) * 2021-01-13 2021-04-30 中国地质科学院 Typhoon area bamboo forest landslide safety coefficient calculation method
CN112733069B (en) * 2021-01-13 2021-12-14 中国地质科学院 Typhoon area bamboo forest landslide safety coefficient calculation method

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