Effects of Rainfall on Soil Temperature, Moisture and Water Movement of Platycladus orientalis on Rocky Hills of North China

TIAN Chao; MENG Ping; ZHANG Jin-song; SUN Shou-jia; HUANG Hui; JIA Chang-rong; LI Jian zhong

Volume 28 Issue 3

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Effects of Rainfall on Soil Temperature, Moisture and Water Movement of Platycladus orientalis on Rocky Hills of North China

1.
State Key Laboratory of Tree Genetics and Breeding, Research Institute of Forestry, Chinese Academy of Forestry, Beijing 100091, China
2.
Co-Innovation Center for Sustainable Forestry in Southern China, Nanjing Forestry University, Nanjing Jiangsu 210037, China
3.
Dagou-he National Forest Farm, Jiyuan Henan 454650, China

Received Date: 2014-12-05

Abstract

By using stable isotope techniques, the Platycladus orientalis grown on the rocky hilly area of North China were chosen to investigate air temperature, soil temperature, moisture and δD value in order to discuss the effect of seasonal rainfall on soil temperature, moisture and water movement. The results indicated that: the soil temperature following rainfal decreased first and then increased in the rainy season, and decreased with the increases of depths, whereas in the early dry season the temperature continued to decrease but increased with the depth. No matter in the rain or dry season, the soil moisture increased at first and then decreased after the rain, but dropped with the depth of soil. In rain season, when the early soil moisture was low, the low intensity rainfall could further increase the moisture of surface and deep soil and made the water δD value deplete, which showed rainfall could recharge the surface and middle soil. However, in prior plentiful rainfall period, low intensity rainfall could further increased the deep soil moisture, and all the soil water δD value were depleted, which indicated that rainfall could rapidly infiltrate into the deep soil. High intensity rainfall increased all the soil moisture and the increments had small differences, meanwhile all the water δD value were depleted, which showed that rainfall could quickly infiltrate into all the soil. In the early dry season, low intensity rainfall may further increase the surface soil moisture. Even if the prior soil moisture were low, the soil water δD value were all depleted, which pointed that rainfall could rapidly infiltrate into the deep soil and further recharged groundwater. Directly affected by rainfall δD value, the litter water δD value were depleted at first and then enriched. The δD value of spring and groundwater were not affected by short-term rainfall, so they could supply water for plant in the dry season.
- seasonal rainfall,
- soil temperature,
- soil moisture,
- hydrogen stable isotope,
- soil water movement

References

[1]	高红贝, 邵明安. 干旱区降雨过程对土壤水分与温度变化影响研究[J]. 灌溉排水学报, 2011, 30(1):40-45.
[2]	刘颖, 韩士杰, 胡艳玲, 等. 土壤温度和湿度对长白松林土壤呼吸速率的影响[J]. 应用生态学报, 2005, 16(9):1581-1585.
[3]	辛继红, 高红贝, 邵明安. 土壤温度对土壤水分入渗的影响[J]. 水土保持学报, 2009, 23(3):217-220.
[4]	Lee K S, Kim J M, Lee D R, et al. Analysis of water movement through an unsaturated soil zone in Jeju Island, Korea using stable oxygen and hydrogen isotopes[J]. Journal of Hydrology, 2007, 345(3):199-211.
[5]	Löffler J. The influence of micro-climate, snow cover, and soil moisture on ecosystem functioning in high mountains[J]. Journal of Geographical Sciences, 2007, 17(1):3-19.
[6]	Gehrels J C, Peeters J E M, De Vries J J, et al. The mechanism of soil water movement as inferred from¹⁸O stable isotope studies[J]. Hydrological sciences journal, 1998, 43(4):579-594.
[7]	Hillel D. Environmental soil physics: Fundamentals, applications, and environmental considerations[M]. Academic press: San Diego, CA, USA, 1998: 771.
[8]	Stephenson N L. Climatic control of vegetation distribution: the role of the water balance[J]. The American Naturalist, 1990, 135(5): 649-670.
[9]	Ferrio J P, Resco V, Williams D G, et al. Stable isotopes in arid and semi-arid forest systems[J]. Investigation Agraria-Sistemasy Recursos Forestales, 2005, 14(3): 371-382.
[10]	Sala O E, Lauenroth W K, Parton W J, et al. Water status of soil and vegetation in a shortgrass steppe[J]. Oecologia, 1981, 48(3): 327-331.
[11]	Kukowski K R, Schwinning S, Schwartz B F. Hydraulic responses to extreme drought conditions in three co-dominant tree species in shallow soil over bedrock[J]. Oecologia, 2013, 171(4): 819-830.
[12]	Nie Y P, Chen H S, Wang K L, et al. Seasonal water use patterns of woody species growing on the continuous dolostone outcrops and nearby thin soils in subtropical China[J]. Plant and soil, 2011, 341(1-2): 399-412.
[13]	Gehrels J C, Peeters J E M, De Vries J J, et al. The mechanism of soil water movement as inferred from ¹⁸O stable isotope studies[J]. Hydrology Science Journal, 1998, 43(4): 579-594.
[14]	Ellsworth P Z, Williams D G. Hydrogen isotope fractionation during water uptake by woody xerophytes[J]. Plant and Soil, 2007, 291(1-2): 93-107.
[15]	Xu Q, Li H B, Chen J Q, et al. Water use patterns of three species in subalpine forest, Southwest China: the deuterium isotope approach[J]. Ecohydrology, 2011, 4(2): 236-244.
[16]	Reynolds J F, Kemp P R, Ogle K, et al. Modifying the "pulse-reserve" paradigm for deserts of North America: precipitation pulses, soil water, and plant responses[J]. Oecologia, 2004, 141(2): 194-210.
[17]	Gazis C, Feng X. A stable isotope study of soil water: evidence for mixing and preferential flow paths[J]. Geoderma, 2004, 119(1-2): 97-111.
[18]	田立德, 姚檀栋, Tsujimura M, 等. 青藏高原中部土壤水中稳定同位素变化[J]. 土壤学报, 2002, 39(3): 289- 295.
[19]	田日昌, 陈洪松, 宋献方, 等. 湘西北红壤丘陵区土壤水运移的稳定性同位素特征[J]. 环境科学, 2009, 30(9): 2747-2754.
[20]	程立平, 刘文兆. 黄土塬区几种典型土地利用类型的土壤水稳定同位素特征[J]. 应用生态学报, 2012, 23(3): 651-658.
[21]	徐庆, 刘世荣, 安树青, 等. 四川卧龙亚高山暗针叶林土壤水的氢稳定同位素特征[J]. 林业科学, 2007, 43(1): 8-14.
[22]	Xu Q, Liu S R, Wan X C, et al. Effects of rainfall on soil moisture and water movement in a subalpine dark coniferous forest in southwestern China[J]. Hydrological Processes, 2012, 26(25): 3800-3809.
[23]	樊克锋, 杨东潮. 论太行山地貌系统[J]. 长春工程学院学报:自然科学版, 2006, 7(1): 51-53, 62.
[24]	胡淑萍, 余新晓, 岳永杰. 北京百花山森林枯落物层和土壤层水文效应研究[J].水土保持学报, 2008, 22(1): 146-150.
[25]	Snyder K A, Williams D G. Water source used by riparian trees varies among stream types on the San Pedro River, Arizona[J]. Agricultural and Forest Meteorology, 2000, 105(1-3): 227-240.
[26]	崔素芳, 张振华, 姚付启, 等.基于偏相关分析的烟台市土壤温度影响因素及预测模型研究[J]. 山东农业科学, 2010(1): 18-21.
[27]	孙庆艳, 余新晓, 杨新兵, 等. 密云水库集水区防护林不同树种林冠截留研究[J]. 中国水土保持科学, 2009, 7(3): 73-78.
[28]	Cheng X L, An S Q, Li B, et al. Summer rain pulse size and rainwater uptake by three dominant desert plants in a desertified grassland ecosystem in northwestern China[J]. Plant Ecology, 2006, 184(1): 1-12.
[29]	李润春, 张秀芝, 高俊寿, 等. 山西省代表站不同土层逐旬土壤相对湿度预报模型[J]. 中国农业气象, 2009, 30(3):354-359.
[30]	Reynolds J F, Kemp P R, Ogle K, et al. Modifying the"pulse-reserve"paradigm for deserts of North America: precipitation pulses, soil water, and plant responses[J]. Oecologia, 2004, 141(2): 194-210.
[31]	Loik M E, Breshears D D, Lauenroth W K, et al. A multi-scale perspective of water pulses in dryland ecosystems: climatology and ecohydrology of the western USA[J]. Oecologia, 2004, 141(2): 269-281.
[32]	Gazis C, Feng X. A stable isotope study of soil water: evidence for mixing and preferential flow paths[J]. Geoderma, 2004, 119(1-2): 97-111.

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通讯作者: 陈斌, bchen63@163.com

1.
沈阳化工大学材料科学与工程学院沈阳 110142

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Effects of Rainfall on Soil Temperature, Moisture and Water Movement of Platycladus orientalis on Rocky Hills of North China

1. State Key Laboratory of Tree Genetics and Breeding, Research Institute of Forestry, Chinese Academy of Forestry, Beijing 100091, China

2. Co-Innovation Center for Sustainable Forestry in Southern China, Nanjing Forestry University, Nanjing Jiangsu 210037, China

3. Dagou-he National Forest Farm, Jiyuan Henan 454650, China

Received Date: 2014-12-05

Abstract: By using stable isotope techniques, the Platycladus orientalis grown on the rocky hilly area of North China were chosen to investigate air temperature, soil temperature, moisture and δD value in order to discuss the effect of seasonal rainfall on soil temperature, moisture and water movement. The results indicated that: the soil temperature following rainfal decreased first and then increased in the rainy season, and decreased with the increases of depths, whereas in the early dry season the temperature continued to decrease but increased with the depth. No matter in the rain or dry season, the soil moisture increased at first and then decreased after the rain, but dropped with the depth of soil. In rain season, when the early soil moisture was low, the low intensity rainfall could further increase the moisture of surface and deep soil and made the water δD value deplete, which showed rainfall could recharge the surface and middle soil. However, in prior plentiful rainfall period, low intensity rainfall could further increased the deep soil moisture, and all the soil water δD value were depleted, which indicated that rainfall could rapidly infiltrate into the deep soil. High intensity rainfall increased all the soil moisture and the increments had small differences, meanwhile all the water δD value were depleted, which showed that rainfall could quickly infiltrate into all the soil. In the early dry season, low intensity rainfall may further increase the surface soil moisture. Even if the prior soil moisture were low, the soil water δD value were all depleted, which pointed that rainfall could rapidly infiltrate into the deep soil and further recharged groundwater. Directly affected by rainfall δD value, the litter water δD value were depleted at first and then enriched. The δD value of spring and groundwater were not affected by short-term rainfall, so they could supply water for plant in the dry season.

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Reference (32)

[1]	高红贝, 邵明安. 干旱区降雨过程对土壤水分与温度变化影响研究[J]. 灌溉排水学报, 2011, 30(1):40-45.
[2]	刘颖, 韩士杰, 胡艳玲, 等. 土壤温度和湿度对长白松林土壤呼吸速率的影响[J]. 应用生态学报, 2005, 16(9):1581-1585.
[3]	辛继红, 高红贝, 邵明安. 土壤温度对土壤水分入渗的影响[J]. 水土保持学报, 2009, 23(3):217-220.
[4]	Lee K S, Kim J M, Lee D R, et al. Analysis of water movement through an unsaturated soil zone in Jeju Island, Korea using stable oxygen and hydrogen isotopes[J]. Journal of Hydrology, 2007, 345(3):199-211.
[5]	Löffler J. The influence of micro-climate, snow cover, and soil moisture on ecosystem functioning in high mountains[J]. Journal of Geographical Sciences, 2007, 17(1):3-19.
[6]	Gehrels J C, Peeters J E M, De Vries J J, et al. The mechanism of soil water movement as inferred from¹⁸O stable isotope studies[J]. Hydrological sciences journal, 1998, 43(4):579-594.
[7]	Hillel D. Environmental soil physics: Fundamentals, applications, and environmental considerations[M]. Academic press: San Diego, CA, USA, 1998: 771.
[8]	Stephenson N L. Climatic control of vegetation distribution: the role of the water balance[J]. The American Naturalist, 1990, 135(5): 649-670.
[9]	Ferrio J P, Resco V, Williams D G, et al. Stable isotopes in arid and semi-arid forest systems[J]. Investigation Agraria-Sistemasy Recursos Forestales, 2005, 14(3): 371-382.
[10]	Sala O E, Lauenroth W K, Parton W J, et al. Water status of soil and vegetation in a shortgrass steppe[J]. Oecologia, 1981, 48(3): 327-331.
[11]	Kukowski K R, Schwinning S, Schwartz B F. Hydraulic responses to extreme drought conditions in three co-dominant tree species in shallow soil over bedrock[J]. Oecologia, 2013, 171(4): 819-830.
[12]	Nie Y P, Chen H S, Wang K L, et al. Seasonal water use patterns of woody species growing on the continuous dolostone outcrops and nearby thin soils in subtropical China[J]. Plant and soil, 2011, 341(1-2): 399-412.
[13]	Gehrels J C, Peeters J E M, De Vries J J, et al. The mechanism of soil water movement as inferred from ¹⁸O stable isotope studies[J]. Hydrology Science Journal, 1998, 43(4): 579-594.
[14]	Ellsworth P Z, Williams D G. Hydrogen isotope fractionation during water uptake by woody xerophytes[J]. Plant and Soil, 2007, 291(1-2): 93-107.
[15]	Xu Q, Li H B, Chen J Q, et al. Water use patterns of three species in subalpine forest, Southwest China: the deuterium isotope approach[J]. Ecohydrology, 2011, 4(2): 236-244.
[16]	Reynolds J F, Kemp P R, Ogle K, et al. Modifying the "pulse-reserve" paradigm for deserts of North America: precipitation pulses, soil water, and plant responses[J]. Oecologia, 2004, 141(2): 194-210.
[17]	Gazis C, Feng X. A stable isotope study of soil water: evidence for mixing and preferential flow paths[J]. Geoderma, 2004, 119(1-2): 97-111.
[18]	田立德, 姚檀栋, Tsujimura M, 等. 青藏高原中部土壤水中稳定同位素变化[J]. 土壤学报, 2002, 39(3): 289- 295.
[19]	田日昌, 陈洪松, 宋献方, 等. 湘西北红壤丘陵区土壤水运移的稳定性同位素特征[J]. 环境科学, 2009, 30(9): 2747-2754.
[20]	程立平, 刘文兆. 黄土塬区几种典型土地利用类型的土壤水稳定同位素特征[J]. 应用生态学报, 2012, 23(3): 651-658.
[21]	徐庆, 刘世荣, 安树青, 等. 四川卧龙亚高山暗针叶林土壤水的氢稳定同位素特征[J]. 林业科学, 2007, 43(1): 8-14.
[22]	Xu Q, Liu S R, Wan X C, et al. Effects of rainfall on soil moisture and water movement in a subalpine dark coniferous forest in southwestern China[J]. Hydrological Processes, 2012, 26(25): 3800-3809.
[23]	樊克锋, 杨东潮. 论太行山地貌系统[J]. 长春工程学院学报:自然科学版, 2006, 7(1): 51-53, 62.
[24]	胡淑萍, 余新晓, 岳永杰. 北京百花山森林枯落物层和土壤层水文效应研究[J].水土保持学报, 2008, 22(1): 146-150.
[25]	Snyder K A, Williams D G. Water source used by riparian trees varies among stream types on the San Pedro River, Arizona[J]. Agricultural and Forest Meteorology, 2000, 105(1-3): 227-240.
[26]	崔素芳, 张振华, 姚付启, 等.基于偏相关分析的烟台市土壤温度影响因素及预测模型研究[J]. 山东农业科学, 2010(1): 18-21.
[27]	孙庆艳, 余新晓, 杨新兵, 等. 密云水库集水区防护林不同树种林冠截留研究[J]. 中国水土保持科学, 2009, 7(3): 73-78.
[28]	Cheng X L, An S Q, Li B, et al. Summer rain pulse size and rainwater uptake by three dominant desert plants in a desertified grassland ecosystem in northwestern China[J]. Plant Ecology, 2006, 184(1): 1-12.
[29]	李润春, 张秀芝, 高俊寿, 等. 山西省代表站不同土层逐旬土壤相对湿度预报模型[J]. 中国农业气象, 2009, 30(3):354-359.
[30]	Reynolds J F, Kemp P R, Ogle K, et al. Modifying the"pulse-reserve"paradigm for deserts of North America: precipitation pulses, soil water, and plant responses[J]. Oecologia, 2004, 141(2): 194-210.
[31]	Loik M E, Breshears D D, Lauenroth W K, et al. A multi-scale perspective of water pulses in dryland ecosystems: climatology and ecohydrology of the western USA[J]. Oecologia, 2004, 141(2): 269-281.
[32]	Gazis C, Feng X. A stable isotope study of soil water: evidence for mixing and preferential flow paths[J]. Geoderma, 2004, 119(1-2): 97-111.

Effects of Rainfall on Soil Temperature, Moisture and Water Movement of Platycladus orientalis on Rocky Hills of North China

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通讯作者: 陈斌, bchen63@163.com

Proportional views

Effects of Rainfall on Soil Temperature, Moisture and Water Movement of Platycladus orientalis on Rocky Hills of North China

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