Study on Proper Stand Density of Pinus sylvestris var. mongolica Plantation in Sandy Land Based on Stem Sap Flow Velocity

HAN Hui; ZHANG Xue-li; DANG Hong-zhong; XU Gui-jun; ZHANG Bai-xi; YOU Guo-chun

Volume 28 Issue 6

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Study on Proper Stand Density of Pinus sylvestris var. mongolica Plantation in Sandy Land Based on Stem Sap Flow Velocity

1.
Liaoning Institute of Sand Fixation and Afforestation, Fuxin 123000, Liaoning, China
2.
Institute of Desertification Studies, Chinese Academy of Forestry, Beijing 100091, China

Received Date: 2015-01-19

Abstract

The precise determination of transpirational water-consumption is of great significance of the judgement of stand water balance. The present proper density of Pinus sylvestris var. mongolica plantation was calculated by means of water balance based on 5 years' observation of the precipitation, the canopy interception, the forest evapotranspiration, the soil water content and the sap flow velocity(SFV) which was measured by thermal dissipation probe(TDP) during the growing season. The sap flow observation of P. sylvestris var. mongolica in Zhanggutai started in early April and ended in late October, the monthly average SFV during the growing season from April to October were 2.58, 4.78, 5.19, 5.01, 4.84, 4.30 and 1.93 cm·per hour respectively, the highest SFV appeared in June, higher SFV appeared in July, August, May and September successively and lower SFV appeared in April and October. Through calculating, the proper density of P. sylvestris var. mongolica in 14, 16, 18, 20 cm diameter class were 688, 531, 422 and 344 plants per hectare. Over-high density was the common problem existed in pure stands in the same diameter class.
- sap flow velocity,
- Pinus sylvestris var. mongolica,
- Zhanggutai,
- stand density

References

[1]	焦树仁.辽宁章古台樟子松人工林水分动态的研究[J].植物生态学与地植物学学报,1987,11(04)296-307.
[2]	柴永红,田炜煜,张红叶.樟子松在哲里木盟沙地造林的成效[J].内蒙古林业科技,1989,03:16-18+13.
[3]	杨文斌,杨明,任建民.樟子松等人工林土壤水分收支状况及其合理密度的初步研究[J].干旱区资源与环境,1992,(4):47-54.
[4]	苑增武,张庆宏,张延新,等.不同密度樟子松人工林土壤水分变化规律[J].吉林林业科技,2000,29(1):1-4,7.
[5]	赵晓彬.樟子松造林密度与沙层水分的关系研究[J].防护林科技,2004(5):4-5,8.
[6]	张继义,赵哈林,崔建垣,等.科尔沁沙地樟子松人工林土壤水分动态的研究[J].林业科学,2005,41(3):1-6.
[7]	罗玲,廖超英.榆林沙区不同立地条件引种樟子松生长特性的对比研究[J].西北农业学报,2008,17(3):182-185,204.
[8]	原戈.辽宁省沙地樟子松人工林衰退原因与治理对策[J].辽宁林业科技,2000(6):1-4.
[9]	焦树仁.辽宁省章古台樟子松固沙林提早衰弱的原因与防治措施[J].林业科学,2001,37(2):131-138.
[10]	宋晓东,刘桂荣,陈江燕,等.樟子松枯死原因与防治技术研究[J].北华大学学报:自然科学版,2003,4(2):166-169,177.
[11]	曾德慧,姜凤岐,范志平,等.樟子松人工固沙林稳定性的研究[J].应用生态学报,1996,7(4):337-343.
[12]	曾德慧,姜凤歧.从水量平衡角度探讨沙地樟子松人工林的合理密度[J].防护林科技,1995,(1):4-7,26.
[13]	刘朝霞,吕荣,常金宝,等.沙地樟子松人工林适宜初植密度的确定及中龄林期密度调控研究[J].内蒙古林业科技,1998,(1):9-12,33.
[14]	张日升,肖巍,于红军,等.沙地樟子松人工林合理经营密度的研究[J].辽宁林业科技,2014,(4):12-15.
[15]	隋旭红,张建军,文万荣.晋西黄土区辽东栎、山杨树干液流比较研究[J].生态学报, 2011, 31(16):4791-4798.
[16]	党宏忠,李卫,张友焱,等.新疆杨边材贮存水分对单株液流通量的影响[J].生态学报,2012,32(24):7801-7807.
[17]	党宏忠,杨文斌,李卫,等.民勤绿洲二白杨树干液流的径向变化及时滞特征[J].应用生态学报,2014,25(9):2501-2510.
[18]	孙龙,王传宽,杨国亭,等.应用热扩散技术对红松人工林树干液流通量的研究[J].林业科学,2007,43(11):8-14.
[19]	王华田,马履一.利用热扩式边材液流探针(TDP)测定树木整株蒸腾耗水量的研究[J].植物生态学报,2002,26(6):661-667.
[20]	王小菲,孙永玉,李昆,等.干热河谷大叶相思树干液流季节动态及其与气象因子的关系[J].林业科学研究,2013,26(2):145-150.
[21]	党宏忠,张劲松,李卫.柠条主根液流与叶面积关系初探[J].林业科学研究,2009,22(5):635-640.
[22]	蒋文伟,汤富彬,刘志梅,等.天目山柳杉古树的液流特征研究[J].林业科学研究, 2012,25(1):58-64.
[23]	张友焱,周泽福,党宏忠,等.利用TDP茎流计研究沙地樟子松的树干液流[J].水土保持研究,2006,13(4):78-80.
[24]	孙慧珍,赵雨森.水曲柳和樟子松树干液流对不同天气的响应[J].东北林业大学学报,2008,36(1):1-3.
[25]	Granier A. A new method of sap flow measurement in tree stems[J]. Annales of Forest Science, 1985, 42(2):193-200.
[26]	Granier A. Evaluation of transpiration in a Douglas fir stand by means of sap flow measurements[J]. Tree Physiology, 1987,(3):309-320.
[27]	徐海涛.章古台沙地影响樟子松生长主要生态因子的初探[J].辽宁林业科技,1989,(2):20-25,5.
[28]	郭忠升,邵明安.半干旱区人工林草地土壤旱化与土壤水分植被承载力[J].生态学报,2003,23(8):1640-1647.
[29]	郭忠升,邵明安.土壤水分植被承载力研究成果在实践中的应用[J].自然资源学报,2009,(12):2187-2193.
[30]	韩辉,白雪峰,徐贵军,等.章古台地区樟子松人工林水量平衡初步研究[J].辽宁林业科技,2012,(6):8-11,14.
[31]	韩辉,白雪峰,徐贵军,等.章古台樟子松树干液流的密度特征[J].东北林业大学学报,2013,41(4):27-31,82.

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通讯作者: 陈斌, bchen63@163.com

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沈阳化工大学材料科学与工程学院沈阳 110142

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Study on Proper Stand Density of Pinus sylvestris var. mongolica Plantation in Sandy Land Based on Stem Sap Flow Velocity

1. Liaoning Institute of Sand Fixation and Afforestation, Fuxin 123000, Liaoning, China

2. Institute of Desertification Studies, Chinese Academy of Forestry, Beijing 100091, China

Received Date: 2015-01-19

Abstract: The precise determination of transpirational water-consumption is of great significance of the judgement of stand water balance. The present proper density of Pinus sylvestris var. mongolica plantation was calculated by means of water balance based on 5 years' observation of the precipitation, the canopy interception, the forest evapotranspiration, the soil water content and the sap flow velocity(SFV) which was measured by thermal dissipation probe(TDP) during the growing season. The sap flow observation of P. sylvestris var. mongolica in Zhanggutai started in early April and ended in late October, the monthly average SFV during the growing season from April to October were 2.58, 4.78, 5.19, 5.01, 4.84, 4.30 and 1.93 cm·per hour respectively, the highest SFV appeared in June, higher SFV appeared in July, August, May and September successively and lower SFV appeared in April and October. Through calculating, the proper density of P. sylvestris var. mongolica in 14, 16, 18, 20 cm diameter class were 688, 531, 422 and 344 plants per hectare. Over-high density was the common problem existed in pure stands in the same diameter class.

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[1]	焦树仁.辽宁章古台樟子松人工林水分动态的研究[J].植物生态学与地植物学学报,1987,11(04)296-307.
[2]	柴永红,田炜煜,张红叶.樟子松在哲里木盟沙地造林的成效[J].内蒙古林业科技,1989,03:16-18+13.
[3]	杨文斌,杨明,任建民.樟子松等人工林土壤水分收支状况及其合理密度的初步研究[J].干旱区资源与环境,1992,(4):47-54.
[4]	苑增武,张庆宏,张延新,等.不同密度樟子松人工林土壤水分变化规律[J].吉林林业科技,2000,29(1):1-4,7.
[5]	赵晓彬.樟子松造林密度与沙层水分的关系研究[J].防护林科技,2004(5):4-5,8.
[6]	张继义,赵哈林,崔建垣,等.科尔沁沙地樟子松人工林土壤水分动态的研究[J].林业科学,2005,41(3):1-6.
[7]	罗玲,廖超英.榆林沙区不同立地条件引种樟子松生长特性的对比研究[J].西北农业学报,2008,17(3):182-185,204.
[8]	原戈.辽宁省沙地樟子松人工林衰退原因与治理对策[J].辽宁林业科技,2000(6):1-4.
[9]	焦树仁.辽宁省章古台樟子松固沙林提早衰弱的原因与防治措施[J].林业科学,2001,37(2):131-138.
[10]	宋晓东,刘桂荣,陈江燕,等.樟子松枯死原因与防治技术研究[J].北华大学学报:自然科学版,2003,4(2):166-169,177.
[11]	曾德慧,姜凤岐,范志平,等.樟子松人工固沙林稳定性的研究[J].应用生态学报,1996,7(4):337-343.
[12]	曾德慧,姜凤歧.从水量平衡角度探讨沙地樟子松人工林的合理密度[J].防护林科技,1995,(1):4-7,26.
[13]	刘朝霞,吕荣,常金宝,等.沙地樟子松人工林适宜初植密度的确定及中龄林期密度调控研究[J].内蒙古林业科技,1998,(1):9-12,33.
[14]	张日升,肖巍,于红军,等.沙地樟子松人工林合理经营密度的研究[J].辽宁林业科技,2014,(4):12-15.
[15]	隋旭红,张建军,文万荣.晋西黄土区辽东栎、山杨树干液流比较研究[J].生态学报, 2011, 31(16):4791-4798.
[16]	党宏忠,李卫,张友焱,等.新疆杨边材贮存水分对单株液流通量的影响[J].生态学报,2012,32(24):7801-7807.
[17]	党宏忠,杨文斌,李卫,等.民勤绿洲二白杨树干液流的径向变化及时滞特征[J].应用生态学报,2014,25(9):2501-2510.
[18]	孙龙,王传宽,杨国亭,等.应用热扩散技术对红松人工林树干液流通量的研究[J].林业科学,2007,43(11):8-14.
[19]	王华田,马履一.利用热扩式边材液流探针(TDP)测定树木整株蒸腾耗水量的研究[J].植物生态学报,2002,26(6):661-667.
[20]	王小菲,孙永玉,李昆,等.干热河谷大叶相思树干液流季节动态及其与气象因子的关系[J].林业科学研究,2013,26(2):145-150.
[21]	党宏忠,张劲松,李卫.柠条主根液流与叶面积关系初探[J].林业科学研究,2009,22(5):635-640.
[22]	蒋文伟,汤富彬,刘志梅,等.天目山柳杉古树的液流特征研究[J].林业科学研究, 2012,25(1):58-64.
[23]	张友焱,周泽福,党宏忠,等.利用TDP茎流计研究沙地樟子松的树干液流[J].水土保持研究,2006,13(4):78-80.
[24]	孙慧珍,赵雨森.水曲柳和樟子松树干液流对不同天气的响应[J].东北林业大学学报,2008,36(1):1-3.
[25]	Granier A. A new method of sap flow measurement in tree stems[J]. Annales of Forest Science, 1985, 42(2):193-200.
[26]	Granier A. Evaluation of transpiration in a Douglas fir stand by means of sap flow measurements[J]. Tree Physiology, 1987,(3):309-320.
[27]	徐海涛.章古台沙地影响樟子松生长主要生态因子的初探[J].辽宁林业科技,1989,(2):20-25,5.
[28]	郭忠升,邵明安.半干旱区人工林草地土壤旱化与土壤水分植被承载力[J].生态学报,2003,23(8):1640-1647.
[29]	郭忠升,邵明安.土壤水分植被承载力研究成果在实践中的应用[J].自然资源学报,2009,(12):2187-2193.
[30]	韩辉,白雪峰,徐贵军,等.章古台地区樟子松人工林水量平衡初步研究[J].辽宁林业科技,2012,(6):8-11,14.
[31]	韩辉,白雪峰,徐贵军,等.章古台樟子松树干液流的密度特征[J].东北林业大学学报,2013,41(4):27-31,82.

Study on Proper Stand Density of Pinus sylvestris var. mongolica Plantation in Sandy Land Based on Stem Sap Flow Velocity

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通讯作者: 陈斌, bchen63@163.com

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Study on Proper Stand Density of Pinus sylvestris var. mongolica Plantation in Sandy Land Based on Stem Sap Flow Velocity

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