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徐高福, 章德三, 李贺鹏, 余梅生, 柏明娥. 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(5): 1-9. DOI: 10.3969/j.issn.1001-3776.2017.05.001
引用本文: 徐高福, 章德三, 李贺鹏, 余梅生, 柏明娥. 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(5): 1-9. DOI: 10.3969/j.issn.1001-3776.2017.05.001
XU Gao-fu, ZHANG De-san, LI He-peng, YU Mei-sheng, BAI Ming-e. 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(5): 1-9. DOI: 10.3969/j.issn.1001-3776.2017.05.001
Citation: XU Gao-fu, ZHANG De-san, LI He-peng, YU Mei-sheng, BAI Ming-e. 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(5): 1-9. DOI: 10.3969/j.issn.1001-3776.2017.05.001

千岛湖水位变化特征和消落带梯级造林策略研究

Water Level Characteristics and Afforestation at Terraced Field of Hydro-fluctuation Belt in Thousand-island Lake

  • 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.

     

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