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多层级视角下共享单车潮汐模式测度方法

陈文栋,  康洁敏,  李根,  邬岚,  程龙

陈文栋, 康洁敏, 李根, 邬岚, 程龙. 多层级视角下共享单车潮汐模式测度方法[J]. 交通信息与安全, 2026, 44(4): 150-160. doi: 10.3963/j.issn.1674-4861.2026.04.014
引用本文: 陈文栋, 康洁敏, 李根, 邬岚, 程龙. 多层级视角下共享单车潮汐模式测度方法[J]. 交通信息与安全, 2026, 44(4): 150-160. doi: 10.3963/j.issn.1674-4861.2026.04.014
CHEN Wendong, KANG Jiemin, LI Gen, WU Lan, CHENG Long. A Method for Measuring Bicycle-Sharing Tidal Flow Patterns from a Multi-level Perspective[J]. Journal of Transport Information and Safety, 2026, 44(4): 150-160. doi: 10.3963/j.issn.1674-4861.2026.04.014
Citation: CHEN Wendong, KANG Jiemin, LI Gen, WU Lan, CHENG Long. A Method for Measuring Bicycle-Sharing Tidal Flow Patterns from a Multi-level Perspective[J]. Journal of Transport Information and Safety, 2026, 44(4): 150-160. doi: 10.3963/j.issn.1674-4861.2026.04.014

多层级视角下共享单车潮汐模式测度方法

doi: 10.3963/j.issn.1674-4861.2026.04.014
基金项目: 

国家自然科学基金项目 52602575

江苏省自然科学基金项目 BK20250687

江苏高校哲学社会科学研究一般项目 2025SJYB0122

详细信息
    作者简介:

    陈文栋(1995—),博士,讲师. 研究方向: 共享交通时空数据挖掘. E-mail: chenwendong@njfu.edu.cn

    通讯作者:

    李根(1989—),博士,副教授. 研究方向: 交通信息工程及控制、交通安全等. E-mail: ligen@njfu.edu.cn

  • 中图分类号: U491.1

A Method for Measuring Bicycle-Sharing Tidal Flow Patterns from a Multi-level Perspective

  • 摘要: 针对栅格等传统聚合单元在共享单车潮汐模式检测中易引发可塑面积单元问题(modifiable areal unit problem,MAUP),以及大规模路网下检测精度与计算效率难以兼顾等实际情况,研究了“管理子区-路段尺度”多层级视角下的两阶段潮汐测度方法。第一阶段,以路段替代栅格作为基本检测单元,从而规避聚合单元主观划分带来的MAUP干扰;第二阶段,引入Leiden社区发现算法将研究区域划分为若干内部联系紧密的管理子区,使路段尺度下的潮汐模式识别范围由全域收缩至管理子区内部,实现计算复杂度的数量级压缩。以厦门岛共享单车系统为例,对其06:00—10:00时段的潮汐模式进行检测,结果表明: ①在精度方面,两阶段法在“极高”与“较高”精度等级上的检出比例分别为74%、61%,而栅格法约为20%、12%;两阶段法与全域处理法相比计算效率提升66%;②83%的潮汐模式发生在早高峰(07:00—09:00),集中于就业区与住宅区附近,具有明显单向潮汐流特征;③检测出的潮汐模式呈现任意形状与多尺度分布,栅格法通常难以探测,且不同时段潮汐强度差异显著,存在分级调度的必要。本文方法在有效克服MAUP的同时,兼顾了潮汐模式检测效率与识别精度,可有效提升运维可操作性。

     

  • 图  1  厦门岛共享单车用户订单、道路网络和土地利用空间分布

    Figure  1.  Spatial distribution of DBS user orders, road networks and land use on Xiamen island

    图  2  共享单车潮汐模式检测示意图

    Figure  2.  Schematic diagram of DBS tidal pattern detection

    图  3  共享单车管理子区划分结果与订单量分布

    Figure  3.  Results of DBS management subzone division and distribution of order volume

    图  4  基于管理子区划分的12月22日共享单车"黑洞"潮汐模式时空分布

    Figure  4.  Spatiotemporal distribution of shared bike"black hole"tidal patterns on december 22 across management subzones

    图  5  5 d内共享单车"黑洞"、"火山"在不同时段下的土地利用分布(右下角数值表示潮汐模式具体数量)

    Figure  5.  Land use distribution of DBS"black hole"and"volcano"across time periods over five days(Bottom-right values show tidal pattern quantities)

    图  6  5 d内共享单车"黑洞"、"火山"在不同时段下的几何分布

    Figure  6.  Geometric distribution of DBS"black hole"and"volcano"across time periods over five days

    图  7  路段尺度与不同栅格尺度下共享单车12月22日早平峰时段(09:00-10:00)潮汐模式的空间分布

    Figure  7.  Spatial distribution of DBS tidal pattern on road segments and different grids during morning off-peak hour(09: 00-10: 00)

    表  1  5 d内共享单车"黑洞"、"火山"潮汐模式在不同时段分布情况

    Table  1.   Distribution of DBS"black hole"and "volcano"tidal patterns across time periods over five days

    时间段 "黑洞"数量/个(比例/%) "火山"数量/个(比例/%)
    06:00-07:00 41(4) 77(7)
    07:00-08:00 350(34) 404(36)
    08:00-09:00 505(49) 526(47)
    09:00-10:00 137(13) 111(10)
    总计 1033(100) 1118(100)
    下载: 导出CSV

    表  2  5d内共享单车"黑洞"、"火山"潮汐强度在不同时段分布情况

    Table  2.   Tidal intensity of shared bike"black holes"and"volcanoes"across time periods over five days

    时间段 共享单车"黑洞" 共享单车"火山"
    潮汐强度/(veh/h) 数量/个(比例/%) 潮汐强度/(veh/h) 数量/个(比例/%)
    06:00-07:00 轻度$ (\leqslant 92) $ 41 (100) 轻度$ (\leqslant 85) $ 77 (100)
    中度(> 92~270) 0 (0) 中度(> 85~244) 0 (0)
    重度(> 270) 0(0) 重度(> 244) 0 (0)
    轻度$ (\leqslant 92) $ 311 (89) 轻度$ (\leqslant 85) $ 338 (84)
    07:00-08:00 中度(> 92~270) 33(9) 中度(> 85~244) 62 (15)
    重度(> 270) 6 (2) 重度(> 244) 4 (1)
    轻度$ (\leqslant 92) $ 413(82) 轻度$ (\leqslant 85) $ 442 (84)
    08:00-09:00 中度(> 92~270) 73 (14) 中度(> 85~244) 72 (14)
    重度(> 270) 19(4) 重度(> 244) 12 (2)
    轻度$ (\leqslant 92) $ 118(86) 轻度$ (\leqslant 85) $ 107 (96)
    09:00-10:00 中度(> 92~270) 19 (14) 中度(> 85~244) 4 (4)
    重度(> 270) 0(0) 重度(> 244) 0 (0)
    下载: 导出CSV

    表  3  5 d内共享单车早高峰时段(07:00—08:00)潮汐模式检测效率

    Table  3.   Detection efficiency of DBS tidal pattern during morning peak hour(07: 00-08: 00)over five days

    管理子区编号 起讫点数量/个 路段数量/个 时间/min
    #1 4331 4869 8
    #2 5553 3832 17
    #3 4706 4354 13
    #4 4560 3409 9
    #5 4740 2105 6
    #6 3714 1219 4
    #7 3044 1455 8
    #8 183 1233 1
    #9 172 973 1
    研究区域 31003 25171 201
    下载: 导出CSV

    表  4  5 d内共享单车潮汐模式检测精度

    Table  4.   Detection accuracy of DBS tidal pattern over five days

    共享单车"黑洞"模式 共享单车"火山"模式
    精度($ R_{I/T} $) 数量(比例/%) 精度($ R_{I/T} $) 数量(比例/%)
    极高$ (0.9 \sim<1.0) $ 322(31) 极高(> 0~0.1) 299(27)
    较高($ 0.8 \sim<0.9 $) 371(36) 较高(> 0.1~0.2) 484(43)
    一般$ (0.7 \sim<0.8) $ 234(23) 一般(> 0.2~0.3) 258(23)
    合格($ 0.6 \sim<0.7 $) 74(7) 合格(> 0.3~0.4) 54(5)
    不合格(< 0.6) 32(3) 不合格(> 0.4) 23(2)
    总计 1 033(100) 1118(100)
    下载: 导出CSV

    表  5  12月22日早平峰时段(09:00—10:00)潮汐模式精度对比

    Table  5.   Accuracy comparison of tidal patterns during the morning off-peak hours(09: 00-10: 00)on December 22

    精度(RI/T) 共享单车"黑洞"数量(比例/%) 共享单车"火山"数量(比例/%)
    两阶段法 200 m栅格 500 m栅格 1000 m栅格 两阶段法 200 m栅格 500 m栅格 1000 m栅格
    极高 7(21) 22(7) 7(4) 2(2) 3(11) 5(3) 0(0) 0(0)
    较高 18(53) 42(13) 11(6) 4(4) 14(50) 15(9) 5(5) 0(0)
    一般 9(26) 84(26) 42(22) 12(13) 9(32) 20(12) 10(11) 5(14)
    合格 0(0) 70(21) 54(28) 37(40) 2(7) 41(24) 26(28) 6(17)
    不合格 0(0) 110(33) 77(40) 38(41) 0 88(52) 53(56) 24(69)
    下载: 导出CSV
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  • 收稿日期:  2026-02-12
  • 网络出版日期:  2026-11-06

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