Study on the Characteristics and Relationship of Soil Moisture and Litter Fall of Three Vegetation Types in Ai-lao Mountain

doi:10.13466/j.cnki.lyzygl.2022.01.006

Abstract

Abstract:

In the Ai-lao Mountain Nature Reserve,Pu'er City,Yunnan Province,this research selected three vegetation types as the objects,including mid-montane moist evergreen broad-leaved forest,mountain top mossy coppiceforest and secondary forest of Populus Yunnanensis,and measured 10-50cm,70cm,90cm,110cm,130cm and 150cm soil moisture content by TDR time domain reflectometer,collected the dry weight of litter (leaf,branch,flower and fruit,bark,moss lichen and other litter) to analyze soil moisture and litter features of different vegetation types and the relationship between them. The results showed that: 1) The soil moisture,as a whole,was represented by the middle-mountain moist evergreen broad-leaved forest>secondary forest of Populus Yunnanensis>mountain top mossy coppice forest. 2) Litter of 3 vegetation types,except for the dry weight of branches and bark,all had significant differences (P<0.05),and the composition of litter was similar,mainly composed of branches and leaves. 3) In the mid-mountain moist evergreen broad-leaved forest,the soil water content only had a very significant positive correlation with the dry leaf weight (P<0.01);in the mountain top mossy coppice,the soil water content only had the negative correlation with the dry weight of moss lichen,and was positively correlated with other indicators;the soil water content in the secondary forest of Populus yunnanensis was negatively correlated with the dry weight of leaf and moss lichen,and positively correlated with the other indicators. RDA analysis results of moss lichen,leaf dry weight and other litter dry weights had greater influence on the soil moisture content of the three vegetation than the dry weight of flowers,fruits,bark and dead branches;in soil moisture content of mid-montane humid evergreen broad-leaved forest,the fitting effect with the total amount of litter was better than that of the other two,which was y=78.601x+35.374.The cultivation of evergreen broad-leaved forest is conducive to the conservation of soil water resources in the mountains.

Key words: soil water content, vegetation type, litter

CLC Number:

S715
S152.7

ZHU Xiuwen, GUO Zihao, YANG Shuangna, GONG Hede. Study on the Characteristics and Relationship of Soil Moisture and Litter Fall of Three Vegetation Types in Ai-lao Mountain[J]. FOREST RESOURCES WANAGEMENT, 2022, (1): 43-51.

Figures/Tables 8

Tab.1

Fig.1

Fig.2

Fig.3

Fig.4

Fig.5

Fig.6

Tab.2

References 35

[1]	刘家臣. 森林抚育经营在现代林业建设中的意义与途径[J]. 新农业, 2021(20):37.
[2]	Zhang Yongwang, Deng Lei, Yan Weiming, et al. Interaction of soil water storage dynamics and long-term natural vegetation succession on the Loess Plateau,China[J]. Catena, 2016,137:52-60. doi: 10.1016/j.catena.2015.08.016
[3]	胡健, 吕一河, 张琨, 等. 祁连山排露沟流域典型植被类型的水源涵养功能差异[J]. 生态学报, 2016,36(11):3338-3349.
[4]	许宇星, 王志超, 竹万宽, 等. 雷州半岛桉树人工林凋落物量和养分循环研究[J]. 热带亚热带植物学报, 2019,27(4):359-366.
[5]	熊壮, 叶文, 张树斌, 等. 西双版纳热带季节雨林与橡胶林凋落物的持水特性[J]. 浙江农林大学学报, 2018,35(6):1054-1061.
[6]	常宗强, 王金叶, 常学向, 等. 祁连山水源涵养林枯枝落叶层水文生态功能[J]. 西北林学院学报, 2001,16(S0):8-13.
[7]	郑江坤, 王婷婷, 付万全, 等. 川中丘陵区典型林分枯落物层蓄积量及持水特性[J]. 水土保持学报, 2014,28(3):87-91.
[8]	卢洪健, 李金涛, 刘文杰. 西双版纳橡胶林枯落物的持水性能与截留特征[J]. 南京林业大学学报, 2011,35(4):67-73.
[9]	赵鸿雁, 吴钦孝, 刘向东, 等. 森林枯枝落叶层抑制土壤蒸发的研究[J]. 西北林学院学报, 1992(2):14-20.
[10]	赵鑫, 辛一凡, 张应龙, 等. 不同植被类型对毛乌素沙地背风坡土壤水分时空变化的影响[J]. 西北林学院学报, 2021,36(3):36-43.
[11]	Entin J K, Robock A, Vinnikov K Y, et al. Temporal and spatial scales of observed soil moisture variations in the extratropics[J]. Journal of Geophysical Research:Atmospheres, 2000,105(D9):11865-11877. doi: 10.1029/2000JD900051
[12]	尹秋龙, 焦菊英, 寇萌. 极端强降雨条件下黄土丘陵沟壑区不同植被类型土壤水分特征[J]. 自然资源学报, 2015,30(3):459-469.
[13]	周长瑞. 论枯落叶层在山地森林水文作用中的重要性[J]. 森林生态系统研究, 1985(5):239-234.
[14]	郭继勋, 孙刚, 姜世成. 松嫩平原羊草草原凋落物层群落学作用的研究[J]. 植物生态学报, 2000,24(4):473-476.
[15]	李叙勇, 孙继坤, 常直海, 等. 天山森林凋落物和枯枝落叶层的研究[J]. 土壤学报, 1997,34(4):406-417.
[16]	王治国. 林业生态工程学—林草植被建设的理论与实践[M]. 北京: 中国林业出版社, 2000:88-102.
[17]	彭舜磊, 由文辉, 沈会涛. 植被群落演替对土壤饱和导水率的影响[J]. 农业工程学报, 2010,26(11):78-84.
[18]	柳金昊, 信忠保, 沈晗悦, 等. 河北坝上地区不同植被类型土壤持水性能研究[J]. 土壤, 2021,53(4):833-840.
[19]	李晓晶, 李德生, 高为霞, 等. 不同植被类型对沙区土壤持水性的影响[J]. 环境科学与技术, 2013,36(10):107-112.
[20]	钱怡顺, 钱昱含, 徐正会, 等. 云南哀牢山自然保护区蚁科昆虫区系分析[J]. 河南农业大学学报, 2021,55(3):485-494.
[21]	张克映, 张一平, 刘玉洪, 等. 哀牢山降水垂直分布特征[J]. 地理科学, 1994(2):144-151.
[22]	温韩东, 林露湘, 杨洁, 等. 云南哀牢山中山湿性常绿阔叶林20hm²动态样地的物种组成与群落结构[J]. 植物生态学报, 2018,42(4):419-429. doi: 10.17521/cjpe.2017.0272
[23]	巩合德, 杨国平, 鲁志云, 等. 哀牢山常绿阔叶林树种多样性及空间分布格局[J]. 生物多样性, 2011,19(2):143-150. doi: 10.3724/SP.J.1003.2011.08313
[24]	刘佩伶, 张倩媚, 刘效东, 等. 2002-2016年鼎湖山典型森林生态系统土壤含水量数据集[J]. 中国科学数据, 2019,4(4):143-152.
[25]	刘佩伶, 陈乐, 刘效东, 等. 鼎湖山不同演替阶段森林土壤水分时空变异研究[J]. 生态学报, 2021,41(5):1798-1807.
[26]	赵永宏, 刘贤德, 张学龙, 等. 祁连山区亚高山灌丛土壤含水量的空间分布与月份变化规律[J]. 自然资源学报, 2016,31(4):672-681.
[27]	韩汉鹏. 试验统计引论[M]. 北京: 中国林业出版社, 2006:93-98.
[28]	Li Lusheng, Gao Xiaodong, Wu Pute, et al. Soil water content and root patterns in a rain-fed jujube plantation across stand ages on the Loess Plateau of China[J]. Land Degradation and Development, 2017,28(1):207-216. doi: 10.1002/ldr.v28.1
[29]	Brasil J B, Andrade E M D, Palácio H A D Q, et al. Characteristics of precipitation and the process of interception in a seasonally dry tropical forest[J]. Journal of Hydrology:Regional Studies, 2018,19:307-317. doi: 10.1016/j.ejrh.2018.10.006
[30]	赵传普, 徐学选, 高朝侠, 等. 黄土丘陵区不同植被类型下土壤水分动态[J]. 水土保持通报, 2015,35(1):68-72.
[31]	郑江坤, 王婷婷, 付万全, 等. 川中丘陵区典型林分枯落物层蓄积量及持水特性[J]. 水土保持学报, 2014,28(3):87-91.
[32]	赵鸿雁, 吴钦孝, 刘向东. 森林枯枝落叶层抑制土壤蒸发的研究[J]. 西北林学院学报, 1992,7(2):14-20.
[33]	卢洪健, 李金涛, 刘文杰. 西双版纳橡胶林枯落物的持水性能与截留特征[J]. 南京林业大学学报:自然科学版, 2011,35(4):67-73.
[34]	Gong Hede, Zhang Yiping, Lei Yanbao, et al. Evergreen broad leaved forest improves soil water status compared with tea plantation in Ai-lao Mountains,Southwest China[J]. Acta Agriculturae Scandianvica Section B-Plant Soil Science, 2001,61(4):384-388.
[35]	吴钦孝, 刘向东, 苏宁虎, 等. 山杨次生林枯枝落叶蓄积量及其水文作用[J]. 水土保持学报, 1992(1):71-76.

植被类型	中山湿性常绿阔叶林	滇山杨次生林	山顶苔藓矮林
群落高度/m	20~25	15~20	3~10
群落优势种	木果柯(Lithocarpus xylocarpus)、黄心木(Machilus gamblei)、硬壳柯(Lithocarpus hancei)、赤柄紫茎(Stewartia pteropetiolata)等	滇山杨(Populus rotundifolia Griff.var.bonati)、硬壳柯等	石栎(Lithocarpus jingdongensis)、露珠杜鹃(Rhododendron irroratum)等
林龄	约300a	约100a	约200a
土壤类型	山地黄棕壤	山地黄棕壤	山地黄棕壤

指标		山顶矮林凋落物总干重	常绿阔叶林凋落物总干重	滇山杨次生林土壤含水量	滇山杨次生林凋落物总干重	常绿阔叶林土壤含水量	山顶苔藓矮林土壤含水量
山顶苔藓矮林凋落物总干重	R	1	-0.066	0.184	0.411^**	0.277^**	-0.044
山顶苔藓矮林凋落物总干重	P		0.455	0.122	0.000	0.001	0.618
常绿阔叶林凋落物总干重	R		1	-0.228	-0.088	0.169^*	0.128
常绿阔叶林凋落物总干重	P			0.054	0.464	0.048	0.142
滇山杨次生林土壤含水量	R			1	0.147	0.092	0.187
滇山杨次生林土壤含水量	P				0.217	0.442	0.116
滇山杨次生林凋落物总干重	R				1	0.151	0.024
滇山杨次生林凋落物总干重	P					0.206	0.838
常绿阔叶林土壤含水量	R					1	0.144
常绿阔叶林土壤含水量	P						0.099
山顶苔藓矮林土壤含水量	R						1