TY - JOUR
T1 - Understory interception contributed to the convergence of surface runoff between a Chinese fir plantation and a secondary broadleaf forest
AU - Jiang, Miao Hua
AU - Lin, Teng Chiu
AU - Shaner, Pei Jen Lee
AU - Lyu, Mao Kui
AU - Xu, Chao
AU - Xie, Jin Sheng
AU - Lin, Cheng Fang
AU - Yang, Zhi Jie
AU - Yang, Yu Sheng
N1 - Funding Information:
This study was supported by the National Natural Science Foundation of China (Grant No. 31130013 , 31470501 , U1505233 ), and the Program for New Century Excellent Talents in Fujian Province University . We are grateful to Guangshui Chen and Yiqing Li from Fujian Normal University for their valuable advice on experimental design, and to Tingwu Lin, Xiaofei Liu, Weisheng Lin, and Decheng Xiong from Fujian Normal University, and other members from Key Laboratory for Subtropical Mountain Ecology, for their assistance in field and laboratory work. We thank Professor Zongming He of Fujian Agriculture and Forestry University for his help on assessing understory plant diversity and Dr. Craig Martin of University of Kansas for proofreading our manuscript. We also thank the staff at local forest station in Sanming Xinkou for their logistic support. The authors declare no conflict of interests.
Publisher Copyright:
© 2019 Elsevier B.V.
PY - 2019/7
Y1 - 2019/7
N2 - Litter and vegetation under forest canopy (i.e., understory vegetation) are known to reduce soil erosion and contribute substantially to evapotranspiration. However, previous studies rarely examined understory water interception. We conducted a comprehensive study of rainfall partitioning using a water balance equation that included both overstory and understory components in a Chinese fir (Cunninghamia lanceolata) plantation and a nearby naturally regenerated Castanopsis (C. carlesii) forest of similar age in southeastern China. Understory interception was measured by submerging understory components (vegetation and litter) in water for 24 h, which gave an estimate of the amount of water retained (i.e., water holding capacity). The total interception loss of rainfall events (>9.8 mm) that generated surface runoff converged between the two forests, a result of a smaller overstory interception loss (20%) coupled with a greater understory interception loss (14%) in the Chinese fir plantation relative to the Castanopsis forest (overstory 25% and understory 11%). The convergence of the total interception contributed to the convergence of the surface runoff, 1% of the rainfall in both forests. Furthermore, the throughfall partition (78%) was greater whereas the stemflow partition (2%) was smaller in the Chinese fir plantation relative to the Castanopsis forest (throufhfall 70% and stemflow 5%). These patterns in rainfall partitioning could be explained by the greater development of the understory vegetation (hence greater understory interception loss) in the Chinese fir plantation, lower canopy leaf area index (hence smaller overstory interception loss and greater throughfall), and rougher barks (hence smaller stemflow) of Chinese fir trees compared to that of Castanopsis trees. Our study illustrated that a comprehensive evaluation of interception loss must take into account understory components.
AB - Litter and vegetation under forest canopy (i.e., understory vegetation) are known to reduce soil erosion and contribute substantially to evapotranspiration. However, previous studies rarely examined understory water interception. We conducted a comprehensive study of rainfall partitioning using a water balance equation that included both overstory and understory components in a Chinese fir (Cunninghamia lanceolata) plantation and a nearby naturally regenerated Castanopsis (C. carlesii) forest of similar age in southeastern China. Understory interception was measured by submerging understory components (vegetation and litter) in water for 24 h, which gave an estimate of the amount of water retained (i.e., water holding capacity). The total interception loss of rainfall events (>9.8 mm) that generated surface runoff converged between the two forests, a result of a smaller overstory interception loss (20%) coupled with a greater understory interception loss (14%) in the Chinese fir plantation relative to the Castanopsis forest (overstory 25% and understory 11%). The convergence of the total interception contributed to the convergence of the surface runoff, 1% of the rainfall in both forests. Furthermore, the throughfall partition (78%) was greater whereas the stemflow partition (2%) was smaller in the Chinese fir plantation relative to the Castanopsis forest (throufhfall 70% and stemflow 5%). These patterns in rainfall partitioning could be explained by the greater development of the understory vegetation (hence greater understory interception loss) in the Chinese fir plantation, lower canopy leaf area index (hence smaller overstory interception loss and greater throughfall), and rougher barks (hence smaller stemflow) of Chinese fir trees compared to that of Castanopsis trees. Our study illustrated that a comprehensive evaluation of interception loss must take into account understory components.
KW - Chinese fir plantation
KW - Forest conversion
KW - Hydrological cycle
KW - Rainfall partitioning
KW - Understory interception
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U2 - 10.1016/j.jhydrol.2019.04.088
DO - 10.1016/j.jhydrol.2019.04.088
M3 - Article
AN - SCOPUS:85065501954
SN - 0022-1694
VL - 574
SP - 862
EP - 871
JO - Journal of Hydrology
JF - Journal of Hydrology
ER -