Hydrological effects of litter and soil for the coniferous forest in the Chongli district for 2022 Olympic Winter Games,Hebei province
GUO Jianjun1, WANG Jiahuan2, HU Jingxia2,3, YANG Xinbing2
1. Saibei Forest Farm of Zhangjiakou City(State-owned Forest Farm Administration Office of Zhangjiakou City), 075000, Zhangjiakou, Hebei, China; 2. College of Forestry, Hebei Agricultural University, 071000, Baoding, Hebei, China; 3. College of Life and Environmental Sciences, Minzu University of China, 100081, Beijing, China
Abstract:[Background] Chongli district, Zhangjiakou, Hebei province, is the venue for the 2022 Winter Olympic Games, and the construction of the slide may seriously influence the vegetation of the forest area. Accurate assessment of the hydrological effects of litter and soil layer in the coniferous forest may provide data support for the impact of the construction of the Winter Olympic Games venue on the hydrological function of the forest.[Methods] Three artificial pure forests of Larix principis-rupprechtii, Pinus tabulaeformis and Pinus sylvestris var. mongolica were selected to investigate the hydrological effects of litter and soil at Heping Forest Farm in Chongli district. Soaking and cutting ring methods were used to measure the hydrological effect of litter and soil layers, respectively.[Results] 1) The largest litter accumulation was 23.98 t/hm2 in L. principis-rupprechtii. The accumulation amount of the semi-decomposed layer were higher than that of the undecomposed layer in L. principis-rupprechtii and P. tabulaeformis, while contrary result was found in P. sylvestris var. mongolica. 2) The maximum water-holding capacity, effective interception capacity and maximum water-holding rate of the litter were the largest in L. principis-rupprechtii, which were 2.15, 1.72 t/hm2 and 632.95%, respectively. It showed a logarithmic relation between the water-holding capacity and water-holding time, and a power function relationship between litter water-absorbing rate and water-holding time. 3) The largest and smallest soil bulk density were 1.23 and 1.01 g/cm3 in P. sylvestris var. mongolica and L. principis-rupprechtii, respectively. While the largest and smallest total porosity of soil was 62.22% and 43.47% in L. principis-rupprechtii and P. tabulaeformis, respectively. Soil infiltration rate increased with infiltration time as a power function. 4)The sort of total water-holding capacity of the forest land was L. principis-rupprechtii (923.93 t/hm2) > P. sylvestris var. mongolica (744.38 t/hm2) > P. tabulaeformis (655.19 t/hm2).The water-holding capacity of the soil layer accounted for more than 99% of the total water holding capacity.[Conclusions] Our results reveal that the largest and least water conservation capacity are the L. principis-rupprechtii and P. tabulaeformis forests. The findings can provide parameters assessment and data support for evaluating the impact of Winter Olympics site construction on hydrological function of coniferous forests.
郭建军, 王佳欢, 胡静霞, 杨新兵. 2022年冬奥会崇礼赛区针叶林枯落物及土壤水文效应[J]. 中国水土保持科学, 2021, 19(4): 44-50.
GUO Jianjun, WANG Jiahuan, HU Jingxia, YANG Xinbing. Hydrological effects of litter and soil for the coniferous forest in the Chongli district for 2022 Olympic Winter Games,Hebei province. SSWC, 2021, 19(4): 44-50.
MIGUEL A G,JUAN F M,JOSÉ D R. Relevant effects of vegetal cover and litter on the soil hydrological response of two contrasting Mediterranean hillslopes at the end of the dry season (South of Spain)[J]. Hydrological Processes,2012,26(11):1729.
[2]
郑淼. 华北土石山区不同林分类型枯落物及土壤水文生态效应[J].中国水土保持科学,2020,18(2):84. ZHENG Miao. Litter and soil hydro-ecological effects of different stand types in the rocky mountain area of North China[J]. Science of Soil and Water Conservation,2020,18(2):84.
[3]
CHRISTOPHER R B, MARTIN S A. Hydrology of the forest city basin, Mid-Continent, USA:Implications for CO2 sequestration in the St. Peter Sandstone[J].Environmental Earth Sciences,2015,73(4):1409.
[4]
武启骞,王传宽,赵娟,等. 帽儿山2种森林类型凋落物和土壤水文效应[J]. 水土保持学报,2015,29(3):161. WU Qiqian, WANG Chuankuan, ZHAO Juan, et al. Hydrological effects of litter and soil in two forest types in Mao'ershan region[J]. Journal of Soil and Water Conservation, 2015, 29(3):161.
[5]
石媛,鲁绍伟,陈波,等. 河北雾灵山不同密度油松人工林枯落物及土壤水文效应[J]. 水土保持学报,2014,28(3):92. SHI Yuan, LU Shaowei, CHEN Bo, et al. Soil hydrological effects and forest litters of Pinus tabulaeformis plantation in the different densities in Wuling Mountain of Hebei[J]. Journal of Soil and Water Conservation,2014, 28(3):92.
[6]
宋小帅,康峰峰,韩海荣,等. 辽河源典型森林类型的土壤水文效应[J]. 水土保持通报,2015,35(2):101. SONG Xiaoshuai, KANG Fengfeng, HAN Hairong, et al. Soil hydrological effects of typical forest types in upper reaches of Liaohe river[J]. Bulletin of Soil and Water Conservation,2015,35(2):101.
[7]
陈继东,周长亮,李惠丽. 接坝地区9种典型林分类型枯落物层和土壤层水文效应[J]. 水土保持研究,2017,24(6):216. CHEN Jidong, ZHOU Changliang, LI Huili. Hydrological effects of litter and soils in nine forest types of the Jieba Region[J]. Research of Soil and Water Conservation, 2017,24(6):216.
[8]
王谦,孙保平,丁国栋,等. 陕西榆林樟子松人工林土壤及枯落物水文效应[J]. 西北农林科技大学学报:自然科学版,2015,43(8):123. WANG Qian, SUN Baoping, DING Guodong, er al. Hydrological effects of soil and litters in Pinus sylvestris var. mongolica plantations in Yulin,Shanxi[J]. Journal of Northwest A & F University (Nat. Sci. Ed.),2015,43(8):123.
[9]
王会京,王红霞,谢宇光. 太行山不同林型枯落物持水性及生态水文效应研究[J]. 水土保持研究,2016,23(6):135. WAGN Huijing, WANG Hongxia, XIE Yuguang. Hydrology functions and water holding capacity of forest litter in Taihangshan Mountain Area[J]. Research of Soil and Water Conservation, 2016,23(6):135.
[10]
刘斌,鲁绍伟,李少宁,等. 北京西山6种天然纯林枯落物及土壤水文效应[J]. 水土保持学报,2015,29(4):73. LIU Bin, LU Shaowei,LI Shaoning, et al. Hydrological effects of litter and soil of six natural forests in Xishan Mountains Area of Beijing[J]. Journal of Soil and Water Conservation, 2015,29(4):73.
[11]
胡静霞,杨新兵,朱辰光,等. 冀西北地区4种纯林枯落物及土壤水文效应[J]. 水土保持研究,2017,24(4):304. HU Jingxia,YANG Xinbing,ZHU Chenguang, et al. Hydrological effects of litter in four pure forests and soils in Northwest of Hebei province[J]. Research of Soil and Water Conservation, 2017, 24(4):304.