[1]徐高福,章德三,李贺鹏,等.千岛湖水位变化特征和消落带梯级造林策略研究[J].浙江林业科技,2017,37(05):1-9.[doi:10.3969/j.issn.1001-3776.2017.05.001]
 XU Gao-fu,ZHANG De-san,LI He-peng,et al.Water Level Characteristics and Afforestation at Terraced Field of Hydro-fluctuation Belt in Thousand-island Lake[J].Journal of Zhejiang Forestry Science and Technology,2017,37(05):1-9.[doi:10.3969/j.issn.1001-3776.2017.05.001]
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千岛湖水位变化特征和消落带梯级造林策略研究()
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《浙江林业科技》[ISSN:1001-3776/CN:33-1112/S]

卷:
37
期数:
2017年05期
页码:
1-9
栏目:
出版日期:
2017-11-30

文章信息/Info

Title:
Water Level Characteristics and Afforestation at Terraced Field of Hydro-fluctuation Belt in Thousand-island Lake
作者:
徐高福1章德三1李贺鹏2余梅生1柏明娥2
1. 浙江省淳安县新安江开发总公司,浙江 淳安 311700;2. 浙江省林业科学研究院,浙江 杭州 310023
Author(s):
XU Gao-fu1ZHANG De-san1LI He-peng2YU Mei-sheng1BAI Ming-e2
1. Chun’an Xin’anjiang Development Company of Zhejiang, Chun’an 311700, China; 2. Zhejiang Academy of Forestry, Hangzhou 310023, China
关键词:
千岛湖消落带水位变化梯级造林
Keywords:
Thousand-island Lake hydro-fluctuation belt water level change afforestation at terraced field
分类号:
S725.1
DOI:
10.3969/j.issn.1001-3776.2017.05.001
文献标志码:
A
摘要:
对浙江省千岛湖1960-2016 年的水位变化、降水量、蒸发量以及2008-2016 年间日水位变化进行分析。结果表明,千岛湖水位历史最高达108.41 m,最低为80.00 m,水位落差由早期(建库20 a 内)的26.69 m 逐渐降至中期(建库21 ~ 40 a)的22.09 m,2000 年以来降至14.14 m。月均水位在1-12 月呈先下降后上升再下降的变化规律,2 月最低,7 月最高;1-3 月为枯水期,6-10 月为丰水期,其他月为平水期。水位变化受降水量、蒸发量及人为等多种因素影响。2016 年冬至2017 年春,分析消落带自然植被分布的影响因素,选择银叶柳Salix chienii,池杉Taxodium ascendens,水杉Metasequoia glyptostroboides,水紫树Nyssa aquatica,枫香树Liquidambar formosana,枫杨Pterocarya stenoptera 大苗在消落带进行梯级造林实践,取得成功。推荐银叶柳,池杉,水杉,水松Glyptostrobuspensilis,中山杉Taxodium‘Zhongshanshan’,水紫树,枫香树,枫杨大苗在消落带种植,梯级造林的海拔高度不宜低于100 m。建议梯级造林技术在千岛湖等土层相对深厚的残积坡土消落带造林时应进行中试。
Abstract:
Analysis were made on annual water level variation, precipitation evaporation during 1960-2016, as well as on daily water level variationduring 2008-2016 in Thousand-island Lake, Zhejiang province. The results showed that the maximum water level was 108.41 m, and the lowest was80.00 m. The mean water level fall of the reservoir was 26.69 m from 1959 to 1979, 22.09 m from 1980 to 1999, and 14.14 m from 2000 to 2016.Mean monthly water level decreased first, then gradually increased and decreased from January to December during 1960-2016, with the lowest inFebruary, and the highest in July. The withered water period of the reservoir was from January to March, wet season from June to October, and theleft months normal. The change of water level had been affected by precipitation, evaporation and human activities. Based on analysis on naturalvertical plant distribution, experiments were conducted from the winter of 2016 to the spring of 2017 on planting saplings of Salix chienii,Taxodiumascendens, Metasequoia glyptostroboides, Nyssa aquatic, Liquidambar formosana, Pterocarya stenoptera at terraced field of the lake. Investigationsshowed that trees were survived and plantation should be higher than 100 m of water level in the lake. The technique for afforestation at terraced fieldaround the lake could be extended for similar places in Thousand-island Lake.

参考文献/References:

[1] 徐高福. 千岛湖森林健康经营实证研究[M]. 杭州:浙江科学技术出版社,2014,222-223.
[2] 徐高福,卢刚,刘乐群,等. 消落带研究现状与建设展望[J]. 绿色科技,2014(9):116-118.
[3] 刘永,郭怀诚,周丰,等. 湖泊水位变动对水生植被的影响机理及其调控方法[J]. 生态学报,2006,26(9):3117-3126.
[4] Naiman R J,Decamps H. The ecology of interfaces: riparian zones[J]. Ann Rev Ecol Syst,1997,28(1):621-658.
[5] Flynn K M,Mendelssohn I A,Wilsey B J. The effect of water level management on the soils and vegetation of two coastal Louisiana marshes[J].Wetland Ecol Manag,1999,7(4):193-218.
[6] Wantzen K M,Rothhaupt K O,M?rtl M,et al. Ecological effects of water-level fluctuations in lakes: an urgent issue[J]. Hydrobiologia,2008,613(1):1-4.
[7] Furey P C,Nordin R N,Mazumder A. Water level drawdown affects physical and biogeochemical properties of littoral sediments of a reservoirand a natural lake[J]. Lake Reserv Manag,2004,20(4):280-295.
[8] Riis T,Hawes I. Relationships between water level fluctuations and vegetation diversity in shallow water of New Zealand lakes[J]. Aquat Bot,2002,74(2):133-148.
[9] 孟熊,廖小红,黎昔春. 洞庭湖水位变化特性及影响研究[J]. 2014,45(13):17-21.
[10] 刘万千,钱湛,张双虎. 洞庭湖水位变化趋势及原因分析[J]. 中国防汛抗旱,2016,26(4):51-54.
[11] 张鑫,吴艳红,张鑫. 1972-2012 年青藏高原中南部内陆湖泊的水位变化[J]. 地理学报,2014,69(7):993-1001.
[12] 丁庆章,刘学勤,张晓可. 水位波动对长江中下游湖泊湖滨带底质环境的影响[J]. 湖泊科学,2014,26(3):340-348.
[13] 姚鑫,杨桂山,万荣荣,等. 水位变化对河流、湖泊湿地植被的影响[J]. 湖泊科学,2014,26 6):813-821.
[14] 杨娇,厉恩华,蔡晓斌,等. 湿地植物对水位变化的响应研究进展[J]. 湿地科学,2014,12(6):807-813.
[15] 李强,宋力,王书敏,等. 水位变化对三峡库区消落带狗牙根种群营养特征的影响[J]. 生态科学,2015, 34(4):15-20.
[16] 蔡壬候,章绍尧. 浙江省植被分片介绍[J]. 植物生态学与地植物学丛刊,1985,9(1):71-76
[17] 徐高福,张立功,余觉来,等. 千岛湖区森林植物资源及其生态经济效益[J]. 林业调查规划,2005,30(增刊):21-23。
[18] 徐高福,卢刚,张建和,等. 千岛湖风化基岩消落带植被的垂直分布特征[J]. 南京林业大学学报(自然科学版),2017,41(3):86-94.
[19] 徐高福,李贺鹏,张建和,等. 千岛湖消落带水位变化对池杉人工林生长的影响[J]. 浙江林业科技,2016,36(5):13-19.
[20] 徐高福,卢刚,张建和,等. 千岛湖库区消落带造林技术研究[J]. 浙江林业科技,2016,36(6):1-7.
[21] Hofmann H,Lorke A,Peeters F. Temporal scales of water-level fluctuations in lakes and their ecological implications[J]. Hydrobiologia,2008,613(1):85-96.
[22] 吴起鑫,韩贵琳,唐杨. 水位变化对湖泊(水库)消落带生态环境影响的研究进展[J]. 地球与环境,2009,37(4):446-453.
[23] 王玉新. 水库水位变动规律及养鱼水面的合理确定[J]. 淡水渔业,1978(4):7-11.
[24] 周华文,张庚然. 新安江水电站工程概况[J]. 大坝与安全,1993,25(3):12-15.
[25] 杜强强,朱航威. 浅析闲林水库在千岛湖引水工程中的地位与作用[J]. 水利建设与和管理,2014(6):66-69.
[26] 倪汉根,杨玉庆. 消除进水口前旋涡漏斗的一个方法[J]. 水利学报,1986(12):47-48.
[27] 徐高福,卢刚,刘乐群,等. 千岛湖消落带湿地植被重建探析[J]. 浙江林业科技,2014,34(6):89-92.
[28] 依俊楠,赵新华,李福钢. 新安江水库供水后调度图优化研究[J]. 水利水电技术,2017,48(2):113-117.
[29] 殷云龙,於朝广,华建峰,等. 重庆万州三峡库区消落带中山杉造林试验[J]. 林业科技开发,2014,28(2):117-121.
[30] 韩路弯,施钦,宣磊,等. 淹水胁迫下中山杉及落羽杉的生长特性研究[J]. 浙江林业科技,2017,37(3):1-8.

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备注/Memo

备注/Memo:
收稿日期:2017-04-07 ;修回日期:2017-09-15基金项目:杭州市社会发展科技计划项目“库区残坡积土消落带湿地森林建设技术研究”(编号:201713)作者简介:徐高福,教授级高级工程师,从事风景园林与森林经营技术工作;E-mail:caxajkfz@163.com。
更新日期/Last Update: 2017-10-20