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. 2017 Feb 16;7:41861. doi: 10.1038/srep41861

Table 4. Elemental concentrations (micro-PIXE, μg g−1 dry weight) in the morphological structures of the roots of Phyllanthus balgooyi, Phyllanthus securinegioides and Rinorea bengalensis.

  Ni Si P S Cl K Ca Mn Fe Co Cu Zn
Phyllanthus balgooyi
 Whole area 120 (4) 2600 (180) 100 (16) 1310 (40) 5040 (12) 6870 (50) 410 (23) 29 (3) 710 (15) 7 (3) 3.1 (0.5) 10.4 (0.7)
 Epidermis 180 (14) 35010 (14) <113 1120 (50) 320 (25) 2380 (50) 860 (27) 63 (9) 3540 (50) 17 (12) <15 15 (7)
 Cortex 34 (3) 450 (3) 90 (20) 840 (20) 7780 (20) 7950 (70) 380 (26) 9 (2) 163 (8) <2 <2.1 10 (1)
 Primary phloem 1880 (30) <385 330 (60) 1320 (40) 1550 (30) 10480 (40) 900 (24) 29 (4) <10 9 (5) <22 23 (6)
 Primary xylem 25 (5) <160 230 (36) 610 (40) 890 (30) 4470 (30) 150 (20) <4 <4 <3 <6 <8
Phyllanthus securinegioides
 Whole area 2080 (43) 8170 (470) 240 (32) 2420 (100) 570 (40) 4400 (80) 820 (20) 44 (2) 1230 (20) 6 (4) 6 (2) 113 (2)
 Epidermis 670 (13) 34600 (1500) 75 (24) 1320 (20) 360 (16) 1590 (40) 460 (10) 230 (8) 8330 (110) 50 (13) <11 18 (4)
 Cortex 2910 (50) 1350 (180) 330 (30) 3520 (130) 750 (30) 3300 (50) 250 (10) 24 (3) 440 (7) <3 8 (3) 47 (5)
 Phloem 9250 (120) 190 (40) 450 (50) 5220 (240) 1360 (60) 11960 (120) 3250 (40) 7 (2) 47 (3) 7 (6) 10 (5) 570 (12)
 Xylem 340 (9) 390 (40) 300 (30) 1120 (50) 230 (12) 2700 (20) 280 (9) 2.8 (0.7) 14.7 (0.5) <0.6 2.1 (0.5) 17.7 (0.7)
Rinorea bengalensis
 Whole area 14700 (150) 6310 (650) 130 (23) 1580 (90) 370 (20) 5570 (60) 5460 (50) 25 (2) 920 (15) <5 25 (7) 63 (2)
 Epidermis 270 (8) 11860 (800) 73 (14) 480 (12) 220 (13) 780 (17) 590 (10) 70 (3) 3170 (50) 13 (5) <3 29 (2)
 Cortex 10060 (140) <128 220 (30) 2020 (110) 480 (20) 9460 (130) 5530 (100) 5 (3) 132 (5) <5 21 (8) 23 (4)
 Phloem 56400 (400) <110 93 (25) 1450 (80) 690 (13) 10560 (80) 8410 (60) 33 (3) 67 (2) <11 78 (21) 250 (20)
 Xylem 910 (14) 260 (14) 220 (20) 420 (25) 140 (8) 2660 (20) 1150 (8) 2.6 (0.6) 6.4 (0.5) <0.8 3.6 (0.6) 13.5 (0.8)

The results were obtained from PIXE spectra extracted from regions representing different morphological structures, and analysed using GeoPIXE software. Errors of analysis (±1 σ uncertainty) are shown in brackets.