[1]谢平,李析男,朱勇,等.基于河链结构和LUCC的分布式流域水文模型及径流响应[J].山地学报,2014,(02):154.
　XIE Ping,LI Xinan,ZHU Yong,et al.Runoff Response with Distributed Hydrological Model Based on River Structure and LUCC[J].Mountain Research,2014,(02):154.
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基于河链结构和LUCC的分布式流域水文模型及径流响应()
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《山地学报》[ISSN:1008-2186/CN:51-1516]

卷:
期数:
2014年02期
页码:
154
栏目:
山地研究
出版日期:
2014-02-01

文章信息/Info

Title:
Runoff Response with Distributed Hydrological Model Based on River Structure and LUCC
作者:
谢平;李析男;朱勇;雷旭;张波;
1.武汉大学水资源与水电工程科学国家重点实验室，湖北 武汉 430072；
2.上海勘测设计研究院，上海 200000
Author(s):
XIE Ping;  LI Xi’nan;  ZHU Yong;  LEI Xu;  ZHANG Bo
1. State Key Laboratory of Water Resources and Hydropower Engineering Science, Wuhan University,Wuhan 430072, China;
2. Shanghai Investigation Design & Research Institute, Shanghai 200434, China
关键词:
水资源; 土地利用/覆被变化; 分布式水文模型; 水文水资源效应; 情景分析; 大理河流域
Keywords:
water resource;  land use and land cover change;  distributed watershed hydrological model;  hydrology and water resources effects;  scenario analysis;  Dali River Basin
分类号:
P343，P901
文献标志码:
A
摘要:
为了定量评估土地利用/覆被变化的水文水资源效应,并考虑流域水文效应的空间差异,提出考虑土地利用/覆被变化的分布式流域水文模型。该模型基于Shreve河链概念对流域河网进行单元划分,基于中国科学院土地资源分类系统的一级类型,将流域划分为6种不同土地利用及覆被变化类型;在每一类土地利用及覆被变化面积上,分别考虑蒸发和下渗的差异,并利用蓄满-超渗耦合产流模型计算该面积上的地表径流量和地面以下径流量;利用地貌汇流模型和线性水库模型将每类面积上的地表径流量和地面以下径流量演算至流域出口断面,从而得到流域的水文过程。模型参数包括流域地貌特征参数、产流参数和汇流参数,前者可以根据地理信息系统技术和遥感技术获...
Abstract:
In order to evaluate quantitatively the hydrology and water resources effects of land use and land cover change (LUCC), a distributed watershed hydrological model considering land use and land cover change (ZWHM-LUCC) is developed. In ZWHM-LUCC, divided basin into the units based on Shreve river chain concept, and based on the firstorder type of land resources classifying system of Chinese Academy of Sciences, a basin is divided into six different types of LUCC. On the area of each type of LUCC, considering the difference of evaporation and infiltration respectively, the surface runoff and the runoff below surface are calculated by using runoff yield model coupling of excess infiltration and excess storage. The surface runoff discharge and the runoff below surface discharge of each area are routed to the outlet section of basin by using geomorphology concentration model and linear reservoir model, thus the basin hydrology discharge process is obtained. The model parameters include watershed geomorphologic characteristic parameters, runoff yield parameters and concentration parameters. The former can be obtained by geography information system technology and remote sensing technology, but the latter need to be derived by the optimization method according to watershed hydrological data. According to the daily rainfall, evaporation and discharge data of Dali River Basin during 1980—2000, the parameters of the model were calibrated and verified. The coefficient of water balance (R) is 0.993 and the qualified rate of annual runoff depth (DR) is 100% during calibration period 1986—2000, and the R is 1.230 and the DR is 66.67% during calibration verification 1980—1985. The calculated results indicate that this model has good adaptability in Dali River Basin. Based on the land use/cover situation of Dali river basin, calculated the benchmark runoff depth was 30.36 mm, and divided the scenarios about for future land utilization in Dali river basin, to the benefit of exert kinds of benefits on the unit (or small basin) water and soil conservation planning and water resources planning.

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备注/Memo

备注/Memo:
收稿日期(Received date)：2013-07-11；改回日期(Accepted): 2013-11-05。
基金项目（Foundation item）：国家自然科学基金资助项目（51179131，50979075，50839005，51190094）。[The project is supported by Nalional Natnral Science Foundation of China(No.51179131；50979075；50839005；51190094).]
作者简介（Biography）：谢平（1963-），男，教授，博士生导师，研究方向为变化环境下的水文水资源。[Xie Ping，Ph D.Donctoral Supervisor,mainly engaged in bgdrobgy and wator resources in changing onvironmont.]E-mail: pxie@whu.edu.cn *
通信作者(Corresponding author)：李析男（1985-），男，博士研究生，研究方向为变化环境下的水文水资源。[Li Xi'nan,Ph D,mainly engaged in bydorology and water resources in charging environnant.]E-mail: lixinan1985@126.com
更新日期/Last Update: 1900-01-01