Deep and far sea seabed stability evaluation method based on fuzzy mathematics
A technology of fuzzy mathematics and evaluation methods, applied in data processing applications, geographic information databases, structured data retrieval, etc., can solve problems such as engineering damage, difficult exploration, and few research results
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Embodiment 1
[0042] Embodiment 1 The fuzzy mathematics-based deep-sea seabed stability evaluation method provided in this embodiment, the process is as follows figure 1 As shown, it specifically includes the following steps:
[0043] 1. Establishment of an evaluation index system for seabed stability in deep and open seas
[0044] 1. Select the deep sea bottom stability evaluation index
[0045] Select the influencing factors that affect the stability of the deep-sea seabed, and obtain the stability evaluation factor set A. The evaluation indicators are mainly composed of two indicators: disaster-forming background and disaster-geology. Factor and sediment four indicators.
[0046] 2. Analyze the degree of attribution of each indicator (influencing factor) to the stability assessment level, and assign a value within the range of 0-1 to each indicator in combination with expert experience and fuzzy mathematics.
[0047] 2. Empower the influencing factors
[0048] Since each influencing ...
Embodiment 2
[0064] Embodiment 2 In this embodiment, the following research area is taken as an example, and the method for evaluating the stability of the deep seabed based on fuzzy mathematics provided by the present invention is used for evaluation. The specific steps are described in detail as follows:
[0065] 1. Overview of the study area, determination of the indicator system and data preparation:
[0066] 1. Overview of the study area
[0067] Such as figure 2 As shown, the study area is located in the southern part of the Philippine Sea in the western Pacific Ocean, at the junction of the Eurasian plate and the Pacific plate, with an area of about 2.6×104km 2 , the seabed elevation is between -6700—-1700m. The tectonic movement is active, the terrain and landform fluctuate greatly, and the seabed micro-geomorphology units are widely developed.
[0068] 2. Selection of evaluation indicators
[0069] According to the actual situation of the study area, the selected geological...
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