Soil particle distribution and water infiltration characteristics during vegetation succession in Phyllostachys edulis stands

doi:10.12302/j.issn.1000-2006.202205039

JOURNAL OF NANJING FORESTRY UNIVERSITY ›› 2024, Vol. 48 ›› Issue (3): 108-116.doi: 10.12302/j.issn.1000-2006.202205039

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Soil particle distribution and water infiltration characteristics during vegetation succession in Phyllostachys edulis stands

XIE Yanyan¹^,²(), GUO Ziwu¹^,^*(), LIN Shuyan², ZUO Keyi¹, YANG Liting¹, XU Sen¹, GU Rui¹, CHEN Shuanglin¹

1. Research Institute of Subtropical Forestry, Chinese Academy of Forestry, Hangzhou 311400, China
2. Bamboo Research Institute, Nanjing Forestry University, Nanjing 210037, China

Received:2022-05-20 Revised:2023-04-30 Online:2024-05-30 Published:2024-06-14

Abstract

Abstract:

【Objective】 The particle size composition, distribution, and water infiltration capability of soil in different soil layers of Phyllostachys edulis stands were measured. The response of soil particle size distribution and water infiltration capability to understory vegetation succession was revealed, which provides guidance for soil ecological management and vegetation renewal of P. edulis stands.【Method】 The understory vegetation successional ages of 21, 9 and 0 years in P. edulis stands were chosen for research. Soil particle size composition and fractal dimension of soil particle volume in different soil layers, as [0, 10) cm, [10, 20) cm, [20, 30) cm of stands land were measured. Soil water infiltration capability was simulated by using Kostiakov, Philip and Horton models. The relationships among soil fractal characteristics, particle composition, and water infiltration capability were analyzed. 【Result】 For P. edulis forests with the same understory successional years, soil clay content, silt content, fractal dimension, and water infiltration capability decreased with the increase of soil depth, while sand content increased gradually. With the extension of vegetation succession years, the content of clay and silt as well as fractal dimension decreased gradually in the [0, 10) cm soil layer, while the sand content increased gradually. The clay and silt contents and fractal dimension in [10, 20) cm and [20, 30) cm soil layers increased first and then decreased, but the sand content changed in the opposite direction. The initial infiltration rate and stable infiltration rate of all soil layers showed an increasing trend with the extension of successional age. Soil fractal dimension was positively correlated with clay particle content, initial infiltration rate, and stable infiltration rate (P<0.05), but negatively correlated with sand particle content (P<0.05). The Kostiakov and Horton models are more suitable for the simulation of soil water infiltration process in experimental P. edulis stands. 【Conclusion】 Vegetation succession under P. edulis stands can significantly improve soil water particle structure and enhance soil water infiltration capability, and the succession time effect is obvious. Soil water infiltration capability of P. edulis in the older 21-year successional understory age was better than that of the younger 9-year and pure bamboo stands.

Key words: Phyllostachys edulis, vegetation succession, soil particle size, fractal characteristic, soil water infiltration capability

CLC Number:

S714

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.

Figures/Tables 8

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References 43

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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
演替年限/a succession year	海拔/m altitude	坡度/ (°) slope	坡向 aspect	土壤类型 soil type	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

演替年限/a succession year	乔木树种 arbor species		灌木树种 shrub species
演替年限/a succession year	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)

变异来源 variation source	df	黏粒 clay		粉粒 silt		砂粒 sand		分形维数 fractal dimension
变异来源 variation source	df	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

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
演替年限/a succession year	土层深度/cm soil depth	黏粒clay	粉粒silt	砂粒sand	分形维数 fractal dimension
	[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

变异来源 variation source	df	初渗率 initialinfiltration rate		稳渗率 stableinfiltration rate
变异来源 variation source	df	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

Soil particle distribution and water infiltration characteristics during vegetation succession in Phyllostachys edulis stands

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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	f_c	R²	f₀	f_c	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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