Chin J Plant Ecol ›› 2012, Vol. 36 ›› Issue (7): 618-628.DOI: 10.3724/SP.J.1258.2012.00618
Special Issue: 稳定同位素生态学
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ZHU Lin1,2,*(), XU Xing1, MAO Gui-Lian3
Published:
2012-07-10
Contact:
ZHU Lin
ZHU Lin, XU Xing, MAO Gui-Lian. Water sources of shrubs grown in the northern Ningxia Plain of China characterized by shallow groundwater table[J]. Chin J Plant Ecol, 2012, 36(7): 618-628.
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URL: https://www.plant-ecology.com/EN/10.3724/SP.J.1258.2012.00618
Fig. 1 Daily precipitation and irrigation from 1 April to 5 July, 2010 in Xidatan. Arrow points to the data when soil water, groundwater, plant xylem water was sampled.
Fig. 3 δ18O and δD of environmental water (A) and plant xylem water (B) sampled at field site and their relationship with arid Northwest China local meteoric water line (ANC LMWL).
土壤水δD Soil water δD 5-28 | 土壤水δ18O Soil water δ18O 5-28 | 土壤水δD Soil water δD 7-4 | 土壤水δ18O Soil water δ18O 7-4 | 土壤含水量 Soil water content 5-28 | 土壤含水量 Soil water content 7-4 | 土壤含盐量 Soil salt content 5-28 | 土壤含盐量 Soil salt content 7-4 | 土壤pH Soil pH 5-28 | 土壤pH Soil pH 7-4 | |
---|---|---|---|---|---|---|---|---|---|---|
土壤水δD Soil water δD 5-28 | 1.00 | |||||||||
土壤水δ18O Soil water δ18O 5-28 | 0.99** | 1.00 | ||||||||
土壤水δD Soil water δD 7-4 | 0.04 | 0.17 | 1.00 | |||||||
土壤水δ18O Soil water δ18O 7-4 | 0.06 | 0.16 | 0.91** | 1.00 | ||||||
土壤含水量 Soil water content 5-28 | -0.66* | -0.69* | -0.23 | -0.16 | 1.00 | |||||
土壤含水量 Soil water content 7-4 | -0.69* | -0.72** | -0.26 | -0.17 | 0.93** | 1.00 | ||||
土壤含盐量 Soil salt content 5-28 | -0.38 | -0.32 | 0.55 | 0.59* | 0.32 | 0.32 | 1.00 | |||
土壤含盐量 Soil salt content 7-4 | 0.02 | 0.08 | 0.58* | 0.59* | 0.27 | 0.12 | 0.71** | 1.00 | ||
土壤pH Soil pH 5-28 | -0.64* | -0.66* | 0.06 | 0.07 | 0.47 | 0.41 | 0.65* | 0.38 | 1.00 | |
土壤pH Soil pH 7-4 | -0.68* | -0.67* | -0.06 | -0.14 | 0.54 | 0.62* | 0.50 | 0.22 | 0.78** | 1.00 |
Table 1 Relationship among soil water hydrogen and oxygen composition, soil water content, soil salt content and pH during different periods in Xidatan shrubberies
土壤水δD Soil water δD 5-28 | 土壤水δ18O Soil water δ18O 5-28 | 土壤水δD Soil water δD 7-4 | 土壤水δ18O Soil water δ18O 7-4 | 土壤含水量 Soil water content 5-28 | 土壤含水量 Soil water content 7-4 | 土壤含盐量 Soil salt content 5-28 | 土壤含盐量 Soil salt content 7-4 | 土壤pH Soil pH 5-28 | 土壤pH Soil pH 7-4 | |
---|---|---|---|---|---|---|---|---|---|---|
土壤水δD Soil water δD 5-28 | 1.00 | |||||||||
土壤水δ18O Soil water δ18O 5-28 | 0.99** | 1.00 | ||||||||
土壤水δD Soil water δD 7-4 | 0.04 | 0.17 | 1.00 | |||||||
土壤水δ18O Soil water δ18O 7-4 | 0.06 | 0.16 | 0.91** | 1.00 | ||||||
土壤含水量 Soil water content 5-28 | -0.66* | -0.69* | -0.23 | -0.16 | 1.00 | |||||
土壤含水量 Soil water content 7-4 | -0.69* | -0.72** | -0.26 | -0.17 | 0.93** | 1.00 | ||||
土壤含盐量 Soil salt content 5-28 | -0.38 | -0.32 | 0.55 | 0.59* | 0.32 | 0.32 | 1.00 | |||
土壤含盐量 Soil salt content 7-4 | 0.02 | 0.08 | 0.58* | 0.59* | 0.27 | 0.12 | 0.71** | 1.00 | ||
土壤pH Soil pH 5-28 | -0.64* | -0.66* | 0.06 | 0.07 | 0.47 | 0.41 | 0.65* | 0.38 | 1.00 | |
土壤pH Soil pH 7-4 | -0.68* | -0.67* | -0.06 | -0.14 | 0.54 | 0.62* | 0.50 | 0.22 | 0.78** | 1.00 |
水分来源 Water source | 灌木种类 Species of shrub | |||||||
---|---|---|---|---|---|---|---|---|
水源的同位素组成 Isotopic composition of water (‰) | 20年生多枝柽柳 20-year-old Tamarix ramosissima | 3年生多枝柽柳 3-year-old T. ramosissima | 3年生宁夏枸杞 3-year-old Lycium barbarum | 3年生四翅滨藜 3-year-old Atriplex canescens | ||||
δ18O | δD | |||||||
5月28日 28 May | 土壤深度 Soil depth (cm) | 0-20 | -5.69 | -42.89 | 5.10 (0-20) | 70.10 (58-81) | 52.30 (35-66) | 48.90 (31-63) |
20-80 | -9.26 | -76.79 | 28.70 (0-95) | 6.60 (0-30) | 10.50 (0-47) | 11.30 (0-50) | ||
80-140 | -8.27 | -71.78 | 15.40 (0-60) | 9.30 (0-42) | 14.70 (0-65) | 15.80 (0-69) | ||
140-200 | -9.47 | -77.00 | 29.40 (0-90) | 6.20 (0-29) | 9.90 (0-44) | 10.60 (0-47) | ||
地下水 Groundwater | -8.70 | -65.93 | 21.50 (0-100) | 7.90 (0-36) | 12.60 (0-55) | 13.40 (0-59) | ||
7月4日 4 July | 土壤深度 Soil depth (cm) | 0-20 | -9.79 | -77.72 | 20.40 (0-90) | 11.00 (0-51) | 11.20 (0-52) | 18.40 (0-82) |
20-80 | -10.11 | -78.66 | 17.50 (0-77) | 9.40 (0-44) | 9.60 (0-45) | 15.80 (0-70) | ||
80-140 | -7.78 | -63.37 | 25.00 (10-39) | 59.50 (49-72) | 58.80 (48-71) | 32.40 (18-46) | ||
140-200 | -9.97 | -79.87 | 18.70 (0-82) | 10.10 (0-47) | 10.30 (0-48) | 16.90 (0-75) | ||
地下水 Groundwater | -10.02 | -75.79 | 18.30 (0-81) | 9.90 (0-46) | 10.00 (0-47) | 16.50 (0-73) |
Table 2 Water uptake rate of potential sources for four shrubs in Xidatan (mean (minimum-maximum)) (%)
水分来源 Water source | 灌木种类 Species of shrub | |||||||
---|---|---|---|---|---|---|---|---|
水源的同位素组成 Isotopic composition of water (‰) | 20年生多枝柽柳 20-year-old Tamarix ramosissima | 3年生多枝柽柳 3-year-old T. ramosissima | 3年生宁夏枸杞 3-year-old Lycium barbarum | 3年生四翅滨藜 3-year-old Atriplex canescens | ||||
δ18O | δD | |||||||
5月28日 28 May | 土壤深度 Soil depth (cm) | 0-20 | -5.69 | -42.89 | 5.10 (0-20) | 70.10 (58-81) | 52.30 (35-66) | 48.90 (31-63) |
20-80 | -9.26 | -76.79 | 28.70 (0-95) | 6.60 (0-30) | 10.50 (0-47) | 11.30 (0-50) | ||
80-140 | -8.27 | -71.78 | 15.40 (0-60) | 9.30 (0-42) | 14.70 (0-65) | 15.80 (0-69) | ||
140-200 | -9.47 | -77.00 | 29.40 (0-90) | 6.20 (0-29) | 9.90 (0-44) | 10.60 (0-47) | ||
地下水 Groundwater | -8.70 | -65.93 | 21.50 (0-100) | 7.90 (0-36) | 12.60 (0-55) | 13.40 (0-59) | ||
7月4日 4 July | 土壤深度 Soil depth (cm) | 0-20 | -9.79 | -77.72 | 20.40 (0-90) | 11.00 (0-51) | 11.20 (0-52) | 18.40 (0-82) |
20-80 | -10.11 | -78.66 | 17.50 (0-77) | 9.40 (0-44) | 9.60 (0-45) | 15.80 (0-70) | ||
80-140 | -7.78 | -63.37 | 25.00 (10-39) | 59.50 (49-72) | 58.80 (48-71) | 32.40 (18-46) | ||
140-200 | -9.97 | -79.87 | 18.70 (0-82) | 10.10 (0-47) | 10.30 (0-48) | 16.90 (0-75) | ||
地下水 Groundwater | -10.02 | -75.79 | 18.30 (0-81) | 9.90 (0-46) | 10.00 (0-47) | 16.50 (0-73) |
Fig. 4 Net photosynthetic rate (Pn), stomatal conductance (Gs), transpiration rate (Tr) and intrinsic water use efficiency (Pn/Gs) of four shrubs measured before irrigation (28 May) and after irrigation (4 July), 2010 (mean ± SD, n = 6). Different lowercases and capital letters represent significant differences among different measuring time (p < 0.05 and p < 0.01), respectively.
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