JOURNAL OF NANJING FORESTRY UNIVERSITY ›› 2024, Vol. 48 ›› Issue (3): 108-116.doi: 10.12302/j.issn.1000-2006.202205039
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XIE Yanyan1,2(), GUO Ziwu1,*(
), LIN Shuyan2, ZUO Keyi1, YANG Liting1, XU Sen1, GU Rui1, CHEN Shuanglin1
Received:
2022-05-20
Revised:
2023-04-30
Online:
2024-05-30
Published:
2024-06-14
CLC Number:
XIE Yanyan, GUO Ziwu, LIN Shuyan, ZUO Keyi, YANG Liting, XU Sen, GU Rui, CHEN Shuanglin. Soil particle distribution and water infiltration characteristics during vegetation succession in Phyllostachys edulis stands[J]. JOURNAL OF NANJING FORESTRY UNIVERSITY, 2024, 48(3): 108-116.
Table 1
Basic situation of Phyllostachys edulis stands with different vegetation succession years"
演替 年限/a succession year | 海拔/m altitude | 坡度/ (°) slope | 坡向 aspect | 土壤 类型 soil type | 毛竹P. edulis | 乔灌木arbor shrubs | ||||
---|---|---|---|---|---|---|---|---|---|---|
立竹密度/ (株·hm-2) bamboo density | 平均 胸径/cm average DBH | 林下植被 密度/ (株·hm-2) understory vegetation density | 平均 株高/m average height | 平均 地径/cm average ground diameter | 郁闭度 conopy density | |||||
0 | 500±10 | 36±2.50 | 西 | 红壤 | 2 625±25 | 9.4±0.60 | — | — | — | 0.60 |
9 | 520±10 | 36±2.50 | 西 | 红壤 | 3 150±30 | 9.2±0.40 | 8 000±55 | 0.76±0.08 | 0.76±0.07 | 0.70 |
21 | 490±10 | 36±2.50 | 西 | 红壤 | 2 275±20 | 8.9±0.40 | 27 511±147 | 2.42±0.20 | 1.69±0.11 | 0.85 |
Table 2
Species composition in Ph. edulis stands with different vegetation succession years"
演替年限/a succession year | 乔木树种 arbor species | 灌木树种 shrub species | ||
---|---|---|---|---|
科Family 属Genus | 主要种main species | 科Family 属Genus | 主要种main species | |
9 | 壳斗科、山茶科、蔷薇科、樟科等9科12属 | 东南石栎(Lithocarpus harlandii)、木荷(Schima superba)、短柄枹栎(Quercus serrata)、老鼠矢(Symplocos stellaris)、苦槠(Castanopsis sclerophylla) | 山茶科、金缕梅科、豆科、杜鹃花科等8科10属 | 柃木(Eurya japonica)、檵木(Loropetalum chinense)、美丽胡枝子(Lespedeza formosa)、马银花(Rhododendron ovatum)、油茶(Camellia oleifera) |
21 | 山茶科、壳斗科、冬青科等7科11属 | 木荷、东南石栎、石栎(Lithocarpus glaber)、苦槠、青冈(Cyclobalanopsis glauca) | 山茶科、杜鹃花科等9科12属 | 柃木、马银花、江南越橘(Vaccinium mandarinorum) |
Table 3
Statistical results of Two-way ANOVA for soil particle composition and fractal dimension in P. edulis stands with different vegetation succession years"
变异来源 variation source | df | 黏粒 clay | 粉粒 silt | 砂粒 sand | 分形维数 fractal dimension | ||||
---|---|---|---|---|---|---|---|---|---|
F | P | F | P | F | P | F | P | ||
演替年限(A) succession years | 2 | 29.965 | <0.01 | 6.897 | <0.05 | 11.254 | <0.01 | 15.254 | <0.01 |
土层深度(D) soil depth | 2 | 46.949 | <0.01 | 12.788 | <0.01 | 19.899 | <0.01 | 28.357 | <0.01 |
演替年限×土层深度(A× D) succession years × soil depth | 4 | 9.457 | <0.01 | 3.937 | <0.05 | 5.289 | <0.05 | 3.969 | <0.05 |
Table 4
Soil particle composition and fractal dimension characteristics in P. edulis stands with different vegetation succession years"
演替年限/a succession year | 土层深度/cm soil depth | 各土壤粒体积百分比/% volume percentage of soil particle | 分形维数 fractal dimension | ||
---|---|---|---|---|---|
黏粒clay | 粉粒silt | 砂粒sand | |||
[0, 10) | 7.02±0.39 Ac | 37.63±3.77 Ac | 55.36±4.15 Aa | 2.66±0.01 Ab | |
21 | [10, 20) | 6.50±0.29 Aa | 33.61±1.42 Aa | 59.90±1.71 Aa | 2.64±0.00 Aa |
[20, 30) | 3.03±0.12 Bb | 30.86±6.01 Aa | 66.11±5.87 Aa | 2.55±0.02 Bb | |
[0, 10) | 9.22±0.08 Ab | 44.21±4.30 Ab | 46.58±4.22 Aa | 2.68±0.01 Ab | |
9 | [10, 20) | 8.51±0.34 Aa | 44.03±6.53 Aa | 47.46±6.82 Aa | 2.68±0.01 Aa |
[20, 30) | 7.50±1.33 Aa | 38.01±3.61 Aa | 54.49±4.28 Ab | 2.65±0.03 Aa | |
[0, 10) | 12.66±0.30 Aa | 57.39±4.71 Aa | 29.95±4.41 Bb | 2.73±0.01 Aa | |
0 | [10, 20) | 7.25±1.57 Ba | 36.97±3.63 Ba | 55.78±5.19 Aa | 2.66±0.03 Aba |
[20, 30) | 5.68±0.33 Ba | 32.56±1.99 Ba | 61.76±1.65 Aab | 2.62±0.02 Ba |
Table 5
Statistical results of Two-way ANOVA for soil initial infiltration rates and stable infiltration rates in P. edulis stands with different vegetation succession years"
变异来源 variation source | df | 初渗率 initialinfiltration rate | 稳渗率 stableinfiltration rate | ||
---|---|---|---|---|---|
F | P | F | P | ||
演替年限(A) succession years | 2 | 29.965 | <0.01 | 6.897 | <0.05 |
土层深度(D) soil depth | 2 | 46.949 | <0.01 | 12.788 | <0.01 |
演替年限×土层深度(A× D) successionyears × soil depth | 4 | 9.457 | <0.01 | 3.937 | <0.05 |
Table 6
Soil infiltration rate and infiltration model parameters in P. edulis stands with different vegetation succession years"
演替 年限/a succession year | 土层 深度/cm soil depth | 初渗率 实测值/ (mm·min-1) initial infiltration rate observed value | 稳渗率 实测值/ (mm·min-1) stable infiltration rate observed value | 入渗模型参数infiltration model parameters | |||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|
Koistakov模型 Koistakov model | Philip模型 Philip model | Horton模型 Horton model | |||||||||||
a | b | R2 | s | fc | R2 | f0 | fc | k | R2 | ||||
[0, 10) | 22.01±0.16 Ab | 15.07±0.85 Aa | 22.92 | 0.09 | 0.964 | 17.16 | 15.05 | 0.813 | 21.97 | 15.03 | 0.05 | 0.982 | |
21 | [10, 20) | 18.83±0.78 Ba | 10.41±0.96 Ba | 18.46 | 0.14 | 0.983 | 20.68 | 9.27 | 0.934 | 18.09 | 10.09 | 0.08 | 0.912 |
[20, 30) | 11.52±1.77 Ca | 4.17±0.50 Ca | 10.99 | 0.23 | 0.980 | 16.49 | 3.37 | 0.994 | 12.37 | 4.54 | 0.19 | 0.950 | |
[0, 10) | 28.20±4.66 Aa | 11.25±1.60 Ab | 28.21 | 0.21 | 0.975 | 40.20 | 9.77 | 0.916 | 25.71 | 11.04 | 0.06 | 0.910 | |
9 | [10, 20) | 15.49±0.34 Bb | 6.52±0.50 Bb | 14.85 | 0.19 | 0.977 | 20.39 | 5.61 | 0.956 | 14.60 | 6.67 | 0.10 | 0.888 |
[20, 30) | 10.58±0.21 Ca | 4.57±0.28 Ca | 10.51 | 0.20 | 0.995 | 14.60 | 3.85 | 0.954 | 10.17 | 4.50 | 0.08 | 0.947 | |
[0, 10) | 7.73±1.63 Ac | 5.29±0.93 Ac | 8.15 | 0.11 | 0.943 | 6.60 | 5.05 | 0.809 | 8.01 | 5.12 | 0.07 | 0.990 | |
0 | [10, 20) | 6.08±0.53 Ac | 4.51±0.37 Ac | 6.46 | 0.09 | 0.870 | 4.11 | 4.50 | 0.672 | 6.21 | 4.10 | 0.04 | 0.991 |
[20, 30) | 3.51±0.64 Bb | 2.05±0.91 Bb | 3.68 | 0.15 | 0.966 | 3.82 | 1.88 | 0.861 | 3.59 | 1.97 | 0.08 | 0.985 |
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