The Impact of Terrain on the Planar Spatial Morphology of Mountain Settlements Studied Using Fractal Dimensions
Abstract
:1. Introduction
Abbreviations
2. Materials and Methods
2.1. Study Area and Sample
2.2. Research Methods
2.2.1. Fractal Dimension
2.2.2. Multiscale Geographically Weighted Regression
2.2.3. Data Preprocessing
3. Results
3.1. Calculation Results of Fractal Dimension for Urban Settlements
3.2. Distribution Results of Spatial Fractal Dimension in Xingdi Village
- Overall, the subspace fractal dimensions of the settlement are predominantly concentrated in its central area, which serves as the core of the settlement. This region retains a diverse array of traditional architecture and fortifications while also representing a transitional zone between old and new structures within the settlement. As one moves toward the periphery of the settlement, there is a noticeable decrease in subspace fractal dimensions. The lowest fractal dimensions can be observed at both the easternmost and northernmost edges of the settlement. Analyzing topographical features reveals that to the southwest, there is a trend towards flatter terrain, whereas to the northeast, it gradually approaches the Mianshan Mountain range. Consequently, subspace fractal dimensions exhibit a radial decline towards this northeastern direction.
- The settlement comprises two distinct parts: new villages and old villages. The boundary between these two areas is located along a main road situated to the south of the settlement, with old villages lying to its north and new villages to its south. Analysis indicates that on average, the subspace fractal dimensions in new village areas exceed those found in old village regions.
- Focusing on specific notable zones within the settlement—such as well-preserved courtyards, fortress walls, and temples—reveals that these locations possess higher covering subregion fractal dimensions compared to their surrounding areas; for instance, regions like Huiluan Temple and East Fort exhibit significantly elevated fractal dimensions relative to nearby locales.
- By overlaying these data with slope maps of the settlement’s terrain (Figure 7), we can derive insights into potential correlations between fractal dimension values and topography. It becomes apparent that in areas characterized by relatively gentle slopes, subspace fractal dimensions tend to be larger; conversely, steeper terrains correspond with lower dimensional values. This observation suggests a possible relationship between topographic features and subspace fractal dimensions—a hypothesis warranting further investigation in subsequent studies.
3.3. MGWR Regression Results
3.3.1. General Effect of MGWR Regression
3.3.2. MGWR Visualization Results
- The regression coefficients are relatively lower in the northwestern part of the settlement and higher in the northeastern part.
- The average value of regression coefficients is higher in steep mountainous regions.
- From the village center to the periphery, the positive impact of elevation on the subspace fractal dimension becomes progressively stronger.
- Both higher and lower elevations exert a stronger positive impact on the subspace fractal dimension of the settlement.
4. Discussion
4.1. Discussion on the Fractal Dimension of Settlements and the Fractal Dimension of Suitable Construction Areas
4.2. Discussion on the Spatial Morphology of Xingdi Village Settlement
4.3. Discussion on Influencing Factors of Subspace Morphology
4.4. Discussion on Development Planning Recommendations
4.4.1. Protection Zoning Based on Fractal Characteristics
4.4.2. Core Construction of Genetic Conservation Systems
5. Conclusions
Limitations
Author Contributions
Funding
Institutional Review Board Statement
Informed Consent Statement
Data Availability Statement
Conflicts of Interest
References
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Village | Architectural Fractal Dimension | Suitable Construction Area Fractal Dimension | Difference |
---|---|---|---|
Dajin | 1.630 | 1.920 | 0.290 |
Xingdi | 1.650 | 1.930 | 0.280 |
Nanzhuang | 1.583 | 1.860 | 0.277 |
Jiaojiabao | 1.585 | 1.850 | 0.265 |
Xiaojin | 1.620 | 1.880 | 0.260 |
Zhangbi | 1.660 | 1.918 | 0.258 |
Xialihou | 1.690 | 1.930 | 0.240 |
Zhang | 1.720 | 1.950 | 0.230 |
Banyu | 1.470 | 1.690 | 0.220 |
Tian | 1.584 | 1.880 | 0.216 |
Liujiashan | 1.590 | 1.790 | 0.200 |
Hongshan | 1.710 | 1.900 | 0.190 |
Architectural Fractal Dimension | Suitable Construction Area Fractal Dimension | |
---|---|---|
Architectural fractal dimension | 1 (0.000 ***) | 0.841 (0.001 ***) |
Suitable construction area fractal dimension | 0.841 (0.001 ***) | 1 (0.000 ***) |
Model Parameter | MGWR |
---|---|
Residual sum of squares | 33.239 |
AIC | 161.880 |
AICc | 165.299 |
R2 | 0.504 |
Adjusted R2 | 0.432 |
p-Value | Mean | STD | Min | Median | Max | |
---|---|---|---|---|---|---|
X1 (Slope) | <0.001 | 0.592 | 0.221 | 0.263 | 0.554 | 0.918 |
X2 (Elevation) | 0.077 | 0.318 | 0.032 | 0.271 | 0.312 | 0.384 |
X3 (Aspect) | 0.335 | 0.051 | 0.010 | 0.034 | 0.051 | 0.067 |
K | 2 | 3 | 4 | 5 | 6 | 7 | 8 |
---|---|---|---|---|---|---|---|
SSE | 83.275802 | 57.619362 | 52.125689 | 45.686388 | 39.778818 | 36.945142 | 34.558358 |
Clustering | |||
---|---|---|---|
1 | 2 | 3 | |
Z-score: fractal dimension | −1.35942 | 0.43210 | 0.25622 |
Z-score: slope | 1.26056 | 0.24549 | −1.14809 |
Z-score: altitude | −0.24554 | −0.76269 | 1.23095 |
Effective | 14 | 31 | 22 |
Invalid | 0 | 0 | 0 |
Clustering | Error | F | Significance | |||
---|---|---|---|---|---|---|
MS | DF | MS | DF | |||
Z-score: fractal dimension | 16.552 | 2 | 0.514 | 64 | 32.204 | <0.001 |
Z-score: slope | 26.557 | 2 | 0.201 | 64 | 131.887 | <0.001 |
Z-score: altitude | 26.106 | 2 | 0.215 | 64 | 121.179 | <0.001 |
Abbreviation | Full Term or Meaning | Unit/Description |
---|---|---|
MGWR | Multiscale Geographically Weighted Regression | A regression model for multiscale analysis |
GIS | Geographic Information System | A system for geographic data analysis |
SPSS | Statistical Package for the Social Sciences | Statistical analysis software |
SSE | Sum of Squared Errors | Used in clustering and regression |
AIC | Akaike Information Criterion | A model selection criterion |
GTWR | Geographically and Temporally Weighted Regression | A regression model considering spatial and temporal effects |
D | Fractal dimension | Indicates spatial filling and complexity |
N(r) | Number of non-empty boxes | A variable in fractal dimension calculations |
r | Box side length | Unit length |
X1 | Ratio of flat terrain | Proportion of areas with 0–5° slope |
X2 | Average elevation | Unit: meters |
X3 | Ratio of south-facing slopes | Proportion of south-facing slope areas |
β0 | Constant term in regression equation | - |
βk | Regression coefficient for the k-th factor | - |
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Pei, S.; Wang, J.; Wang, W. The Impact of Terrain on the Planar Spatial Morphology of Mountain Settlements Studied Using Fractal Dimensions. Appl. Sci. 2025, 15, 3046. https://doi.org/10.3390/app15063046
Pei S, Wang J, Wang W. The Impact of Terrain on the Planar Spatial Morphology of Mountain Settlements Studied Using Fractal Dimensions. Applied Sciences. 2025; 15(6):3046. https://doi.org/10.3390/app15063046
Chicago/Turabian StylePei, Sihang, Jinping Wang, and Wei Wang. 2025. "The Impact of Terrain on the Planar Spatial Morphology of Mountain Settlements Studied Using Fractal Dimensions" Applied Sciences 15, no. 6: 3046. https://doi.org/10.3390/app15063046
APA StylePei, S., Wang, J., & Wang, W. (2025). The Impact of Terrain on the Planar Spatial Morphology of Mountain Settlements Studied Using Fractal Dimensions. Applied Sciences, 15(6), 3046. https://doi.org/10.3390/app15063046