The present study showed that vetiver
could highly accumulate metals Al, Cu, Pb,
Sn and Zn in the upper part of the shoot. Thus,
the vetiver may serve as an important means
for waste water treatment.
The roots and upper parts of shoots
accumulated Al concentration from 17-30
times and 1.2 times higher than “reference
plant”, respectively. Thus, vetiver can be
considered as Al-hyperaccumulation. In other
plants, the excessive or toxic concentration of
Cu is 20-100 mg/kg, but in vetiver plant, it
was much higher and reached up to 660 and
46.2 mg/kg in the roots and shoots,
respectively. Vetiver could withstand and
alive at the Cu concentration of 46 mg/L in
contaminated water. The Pb translocation rate
from root to shoot was up to 41%. Sn highly
accumulated in upper parts with ratio shoot:
root varied from 82 - 277% in the top and
increased to the top by order
S3/R>S2/R>S1/R. Zn could be translocated
from roots and accumulated in the shoots of
vetiver, the ratio shoot to root was up
to 46%
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Vietnam Journal of Earth Sciences, 38(3), 286-296, DOI: 10.15625/0866-7187/38/3/8763
286
(VAST)
Vietnam Academy of Science and Technology
Vietnam Journal of Earth Sciences
Uptake capacity of metals (Al, Cu, Pb, Sn, Zn) by
Vetiveria zizanioides in contaminated water from Dong Xam
metal production trade village, Thai Binh, Vietnam
Nguyen Trung Minh1,*, Seong-Taek Yun2, Jang-Soon Kwon2, Doan Thu Tra3 and Doan
Dinh Hung1
1Vietnam National Museum of Nature (VNMN), Vietnam Academy of Science and Technology
2Department of Earth & Environmental Sciences, Korea University
3Institute of Geological Sciences, Vietnam Academy of Science and Technology, Hanoi, Vietnam
Received 15 November 2014. Accepted 20 August 2016
ABSTRACT
The present study investigates an experiment of uptake capacity of metals by Vetiveria zizanioides to treat
contaminated water from a metal production trade village, Dong Xam, Thai Binh, Vietnam (DXV). Vetiver was
grown in two pot culture experiments TB10, TB6 with solutions containing respective concentrations of Al, Cu, Pb,
Sn and Zn of 2.5, 55.6, 0.15, 7.7 and 24.4 mg from the DXV for a period of 36 days. Vetiver was higher tolerant to
metals Al, Cu, Pb, Sn and Zn than other plant species. The roots (hereafter R) accumulated Al from 17 to 30 folds
than that in “reference plant”. The upper parts of shoots (hereafter S1, S2, and S3) were 1.2 folds higher than that in
“reference plant”. Cu concentrations in the roots and shoots were 660 and 46.2 mg/kg, respectively. Vetiver could
withstand and survive at Cu concentration of 46 mg/L in contaminated water that is markedly higher than other
plants. The translocation of Pb from root to shoot was 41%. Sn accumulated higher in the top, in which shoot/root
ratio varied from 82 to 277%, and increased to the top by order S3/R>S2/R>S1/R. Zn could be translocated from root
and accumulated in shoot. The ratio shoot/root was up to 46%. The present results demonstrated that vetiver was high
tolerant to metals Al, Cu, Pb, Sn and Zn. Therefore, vetiver has a potential phytoremediation of metals in
contaminated soils and wastewaters from trade villages in Vietnam and other countries
Keywords: metals,, Vetiveria zizanioides, trade village Dong Xam, Thai Binh.
©2016 Vietnam Academy of Science and Technology
1. Introduction1
Heavy metal contamination in the
environment by agricultural land erosion,
urban wastes and by-products of rural,
industrial activities and mining industries
attracts worldwide concerns, especially in
*Corresponding author, Email: nttminh@vast.vn
developing countries (Mejare and Bulow,
2001; Tordoff et al., 2000).
Nowadays, there are about thousand trade
villages that are exercising various
professions in Vietnam. However, they are
facing problems with wastewater and solid
waste treatments, particularly, metal
contaminations in wastes.
N.T. Minh, et al./Vietnam Journal of Earth Sciences 38 (2016)
287
The vetiver grass is first grown for soil and
water conservation in farmlands. Vetiver has
unique morphological, physiological and
ecological characteristics, and plays a key role
in the field of environmental protection.
Unique morphological characteristics include
a massive finely structured and deep root
system that can reach up to 3-4 m in the first
year. Vetiver is tolerant to extreme climatic
variation such as prolonged drought, flood,
and extreme temperature. Vetiver can survive
in very harsh environments where surface
temperature varying from -13 °C to 55 °C. It
is also tolerant to a wide range of soil pH,
ranging between 3.0 and 10.5, and soil
salinity, sodicity, acidity, and heavy metals
(Truong, 1996; Truong and Baker, 1998;
Truong and Hart, 2001; Truong and Loch,
2004).
Phylogenetically, vetiver is close to
sorghum. It seems that, as other Panicoideae
plant subfamily, vetiver follows the same
conjugation detoxification pathway (Jensen. et
al., 1977). The major metabolism of atrazine
in vetiver grown in hydroponics was
conjugation, mainly in leaves, a
transformation known to be positive for the
environment (Sylvie et al., 2006).
Vetiver grass was selected for the
wastewater treatment purpose from Dong
Xam metal production trade village, Thai
Binh (DXV) due to many reasons. Firstly, it
can tolerate in the wide range of pollution
conditions, and it has been promoted by
World Bank since 1990 to control soil erosion
throughout the world (Becker, 1992;
Grimshaw, 1989; Steven et al., 1999). Second,
it requires a low cost alternative means to
reduce contaminated areas by heavy metals
(Truong and Baker, 1998). Vetiver grows very
fast with annual productivity of 99 tons/ha, its
strong root system and a long-lived perennial
can survive up to 50 years (Veldkamp, 1999;
Zhang, 1998).
Many previous studies have reported the
uptake capacity of heavy metals by Vetiver
(Adriano, 1992; Chiu et al., 2005, 2006; Lai
and Chen, 2004; Sylvie et al., 2006; Truong
and Baker, 1998; Wilde et al., 2005; Xia,
2004; Yahua et al., 2004; Yang et al., 2003),
but uptake capacities of Al, and Sn have not
been clearly investigated, particularly the
pollution likes in the DXV with number of
metal contaminations.
2. Materials and methods
2.1. Vetiver growth conditions
The soils using for vetiver cultivation were
collected from five points in the study area.
The soils were sieved through a 2-mm mesh
and well mixed to obtain composite
homogeneous samples. Seedling of vetiver
was wrapped in the composite soils, and then
transferred to grown in contaminated waters
with different chemical contents (Figure 1b).
The soils in two pots (TB10, TB6) for
vetiver cultivation were added at the same
amount of metals Al, Cu, Pb, Sn and Zn in
wastewater of DXV at 2.5, 55.6, 0.15, 7.7 and
24.4 mg, respectively. Vetivers were
cultivated in the contaminated solutions with
different concentrations of trace elements
(Table 1) by adding tap water and one pot
(control) was living in the clean tap water. No
fertilizer was applied during the entire
growing period. The temperature in the
laboratory growth chamber was 25 ± 2°C.
After 36 days of growth in laboratory
chamber by contaminated water TB10, TB6
and control water, vetiver plants were
harvested. The plant’s height was 0.7 m
(Figure 1a, b). The plants were first rinsed
three times with tap water to remove all soils
and other materials and then two times with
deionized water. The plants were then dried at
room temperature for five days, then at 80°C
for two days in an electric oven to constant
weight. The plants were sectioned into five
parts: root (R), meristematic region (M) and
Vietnam Journal of Earth Sciences, 38(3), 286-296
288
three parts of shoots (S1 - 10 cm of the shoot
is from the meristematic region, S2- next 10
cm of the shoot, S3- remain part (about 20-
40cm) in the top of the shoot). All samples
were sieved through a 2-mm mesh and well
mixed (Figure 2).
Figure 1. (a) Vetiver grown land and (b) it was grown in laboratory chamber by contaminated water for 36 days
Table 1. Analytical results of contaminated solutions from two wastewater samples from the DXV prior treatment by
vetiver (mean ± SD)
Elements TB10 TB6 Mean, mg/L SD Mean, mg/L SD
Al 1.242 0.002 2.070 0.003
Cu 27.821 0.0009 46.369 0.0015
Pb 0.075 0.0005 0.125 0.0008
Sn 3.861 0.001 6.435 0.001
Zn 12.225 0.0003 20.375 0.0005
2.2 Chemical analysis
Approximately 500 mg plant tissues from
each part of vetiver and standard NIST 1568a
(Rice Flour) were placed into 100 ml Teflon
bottles. The materials were digested at 180°C
with 5ml of 16M HNO3 and 1 ml of 12M HClO4 (5:1 ratio) for 24 hours on a hotplate. After evaporation, the solutions were added
0.03 ml of 18M H2SO4 and kept at 180°C for 24 hours. The dissolved samples were brought
to a volume 30 ml with 2% HNO3.
The concentrations of Al, Cu, Pb, Sn and
Zn in the solutions were determined by ICP
MS at the Korea Basic Science Institute
(KBSI) (Table 1). The standard error (SD) is
calculated from the triplicate analysis (n=3).
The NIST 1568a was used to quantify the
accuracy of metal determination by ICP-MS,
and the recovery levels of Cu, Zn, Cd and
Pb ranged from 90.7 - 104.8% (± 5.0%)
(Table 2).
(a) (b)
N.T. Minh, et al./Vietnam Journal of Earth Sciences 38 (2016)
289
Figure 2. (a) Vetiver samples TB6 and (b) TB10 were sieved through a 2 mm mesh and mixed well
Table 2. Recovery levels of metals for NIST 1568a (Rice Flour)
Element Certificate, mg/kg Found, mg/kg Recovery (%) Mean SD Mean SD Mean SD
Cd 0.022 0.002 0.023 0.0006 104.8 2.6
Cu 2.400 0.3 2.176 0.087 90.7 3.6
Pb <0.010 0.009 0.0005 91.5 5.0
Zn 19.400 0.5 20.301 0.819 104.6 4.2
2.3 Chemical fingerprint
According to Markert (1992), to overcome
the problem of data variation over the scale,
we use chemical fingerprints by normalizing
data to “reference plant” for interpretation and
discussion of Al, Cu, Pb, Sn and Zn
concentrations (Figure 3). The value of
“reference plant” were set to zero
(normalization) and the data of trace metals
Al, Cu, Pb, Sn and Zn concentrations of parts
(a)
(b)
Vietnam Journal of Earth Sciences, 38(3), 286-296
290
of vetiver will be given as deviations from the
value of “reference plant”.
3. Results and discussion
3.1 Aluminum (Al)
The main function of Al in plants is to
control colloidal properties in the cell,
possible activation of some dehydrogenases
and oxidization (Kabata and Pendias, 2001).
The high availability of Al in nutrient soils is
one of the limiting factors in the production of
most field crops (Baker, 1976, Foy et al.,
1978; Frank et al., 1979). The physiological
mechanism of Al toxicity is still debate, but
Al excess in plants is likely to interfere with
cell division and with properties of
protoplasm and cell walls (Foy et al., 1978).
The Al concentration in plants greatly varies,
depending on soil and plant factors.
Chemical fingerprint: The relative
deviation of Al from “reference plant” is
shown in Figure 1a. The concentration of Al
in root tissues was greater than that in the
“reference plant” by 17 to 30 times (Table 4,
Figure 3). The deviation in the lower parts
(meristematic regions M and low parts of
shoots S1) was less than zero, but upper
parts of shoots S2, and S3 was higher,
reaching 120% (TB6-S2). This means that Al
highly concentrated in the top of leave and the
ratio of Al shoot: root varied from 3 up to 8%.
The Al concentration in all parts of vetiver
increased with the contaminated levels of
wastewater (Tables 1 and 3, Figure 4), and
were higher in the roots in comparison to
shoots. The minimum concentration was
found in the meristematic regions, because the
amount of Al passively taken up by roots and
then translocated to tops, reflecting the Al
tolerance of plants. However, it should be
noticed that the ability to accumulate Al in
roots is not necessarily associated with Al
tolerance (Kabata and Pendias, 2001).
Table 3. Concentrations of metals in vetiver parts, (mean ± standard error) (mg/kg)
Sample ID Blank BL1 - Root Blank BL1 - Meristematic region
Blank BL1 -
Shoot S1
Blank BL1 -
Shoot S2
Blank BL1 -
Shoot S3
Element Mean SD Mean SD Mean SD Mean SD Mean SD
Al 1386.78 73.52 14.142 1.029 20.289 4.843 70.735 5.222 52.912 1.724
Cu 9.978 0.448 35.089 1.337 4.460 0.220 3.614 0.180 4.770 0.183
Pb 1.706 0.048 0.039 0.002 0.326 0.012 1.434 0.043 1.627 0.059
Sn 0.306 0.007 0.465 0.026 0.377 0.025 0.444 0.017 0.426 0.028
Zn 33.188 1.301 179.735 8.191 22.612 1.077 19.463 0.842 22.060 0.801
Sample ID TB10 - Root TB10 - Meristematic region TB10 - Shoot S1 TB10 - Shoot S2 TB10 - Shoot S3
Element Mean SD Mean SD Mean SD Mean SD Mean SD
Al 2358.22 26.35 37.619 1.166 88.288 1.784 96.455 2.386 88.158 3.572
Cu 367.833 17.696 84.453 4.491 15.386 0.768 8.189 0.395 11.672 0.474
Pb 1.919 0.071 n.d. n.d. 0.736 0.026 2.860 0.110 1.809 0.055
Sn 0.175 0.010 0.086 0.005 0.160 0.005 0.207 0.012 0.484 0.033
Zn 78.187 4.003 336.966 16.948 23.649 1.108 27.021 1.316 26.628 1.170
Sample ID TB6 - Root TB6 - Meristematic region TB6 - Shoot S1 TB6 - Shoot S2 TB6 - Shoot S3
Element Mean SD Mean SD Mean SD Mean SD Mean SD
Al 2148.32 52.91 41.668 0.604 66.628 6.035 176.675 16.775 106.164 13.811
Cu 660.674 15.220 119.105 4.578 46.151 2.177 13.053 0.471 17.095 0.583
Pb 2.303 0.038 0.117 0.005 1.482 0.042 3.885 0.109 3.245 0.081
Sn 0.333 0.008 0.306 0.016 0.274 0.009 0.501 0.005 0.614 0.024
Zn 141.641 3.777 303.817 12.303 64.808 3.086 47.334 1.971 48.860 1.669
n.d. = not detected
N.T. Minh, et al./Vietnam Journal of Earth Sciences 38 (2016)
291
Figure 3. Relative deviations of vetiver parts after normalization against “reference plant” (Markert B., 1992)
Vietnam Journal of Earth Sciences, 38(3), 286-296
292
Table 4. Relative deviation concentration (%) in parts of vetiver from "reference plant" (Mean ± standard deviation)
Sample vetiver blank BL1
Element R M S1 S2 S3
Al 1633.5 ± 91.9 -82.3 ±1.3 -74.6 ±6.1 -11.6 ±6.5 -33.9 ±2.2
Cu -0.2 ± 4.5 250.9 ±13.4 -55.4 ±2.2 -63.9 ±1.8 -52.3 ±1.8
Pb 70.6 ±4.8 -96.1 ±0.2 -67.4 ±1.2 43.4 ±4.3 62.7 ±5.9
Sn 53.2 ±3.4 132.4 ±13.1 88.4 ±12.6 121.8 ±8.4 112.9 ±14.1
Zn -33.6 ±2.6 259.5 ±16.4 -54.8 ±2.2 -61.1 ±1.7 -55.9 ±1.6
Sample vetiver TB10
Element R M S1 S2 S3
Al 2847.8 ±32.9 -53.0 ±1.5 10.4 ±2.2 20.6 ±3.0 10.2 ±4.5
Cu 3578.3 ±177.0 744.5 ±44.9 53.9 ±7.7 -18.1 ±3.9 16.7 ±4.7
Pb 91.9 ±7.1 -100.0 ±0.2 -26.4 ±2.6 186.0 ±11.0 80.9 ±5.5
Sn -12.5 ±5.1 -56.8 ±2.7 -20.2 ±2.7 3.5 ±5.9 142.2 ±16.7
Zn 56.4 ±8.0 573.9 ±33.9 -52.7 ±2.2 -46.0 ±2.6 -46.7 ±2.3
Sample vetiver TB6
Element R M S1 S2 S3
Al 2585.4 ±66.1 -47.9 ±0.8 -16.7 ±7.5 120.8 ±21.0 32.7 ±17.3
Cu 6506.7 ±152.2 1091.0 ±45.8 361.5 ±21.8 30.5 ±4.7 70.9 ±5.8
Pb 130.3 ±3.8 -88.3 ±0.5 48.2 ±4.2 288.5 ±10.9 224.5 ±8.1
Sn 66.5 ±4.1 52.9 ±7.8 37.1 ±4.4 150.5 ±2.6 207.0 ±12.1
Zn 183.3 ±7.6 507.6 ±24.6 29.6 ±6.2 -5.3 ±3.9 -2.3 ±3.3
3.2. Copper (Cu)
Cu is a component in some enzyme as
catalyst (Schlesinger 2004), involves in
oxidation, photosynthesis, protein and
carbohydrate metabolism, possibly in
symbiotic N2 fixation, and valence changes in
plants (Kabata and Pendias, 2001) (but it is
toxic if concentration of Cu excesses the need
of plants). Cu is an essential element for the
growth of most aquatic organisms but is a
toxic element at concentration of 10 mg/L
(Leckie and Davis, 1979). In our experiment,
vetiver plants were growth well in the
solutions TB10 and TB6 with Cu
concentration of 27.821 and 46.369 mg/L
(Table 1).
In all parts of TB10 and TB6 samples, Cu
concentration was higher in comparison with
vetiver blank (BL1). In each vetiver sample,
Cu concentration is decreased as follows:
R>M>S1> S2, S3 (Table 3; Figure 4b), with
an exception for Blank BL1.
In root tissue, Cu exists entirely in
complexed forms; it is most likely that the
metal enters root cells in dissociated forms
(Kabata and Pendias, 2001) and the same
process occurs in the meristematic regions.
The root and meristematic region tissues had a
strong capability to absorb Cu for reducing
the Cu transport to shoots.
Chemical fingerprint: Cu concentration in
all vetiver parts lived in wastewater was
higher than that of “reference plant”
(exception for TB10-S2, it was slightly lower)
(Table 4; Figure 2). The deviation with
“reference plant” in the shoot it oscillated
from 16.7 (TB10-S3) to 361.5% (TB6-S1), in
the meristematic region from 745 (TB10-M)
to 1091% (TB6-M) and in the root from 3578
(TB10-R) up to 6507 % (TB6-R). On the
contrary, it was negative in the root (-0.2%)
and shoot (-52 -64%) of blank BL1 (except
meristematic region).
The trend of slope line is clearly shown
in Table 4 and Figure 4b, reflecting the
increasing of Cu concentration in
contaminated water. It seems that Cu
concentration in vetiver was the function (in
direct proportion) of its concentration in
contaminated water. Cu concentrations in the
root (R), meristematic region and shoots (S1,
S2, S3) parts of vetiver were all increased
N.T. Minh, et al./Vietnam Journal of Earth Sciences 38 (2016)
293
with its concentration in contaminated water.
The increased level of Cu concentration in
root was faster than in the meristematic region
and in others parts M>S1>S2, S3. Cu has low
mobility relative to other elements in vetiver
and higher Cu concentration remaining in root
and leaf tissues until they senesce (Kabata-
Pendias Alina and Pendias Henryk, 2001). In
other plants, the excessive or toxic
concentration of Cu is 20-100 mg/kg (Kabata
and Pendias, 2001), but Cu concentration
could range from 11 to 660 mg/kg in vetiver
(Table 3).
The ratio of Cu shoot: root was low (4-7%)
for vetiver grown in the wastewater and
higher (36-48%) for vetiver grown in cleaning
water, indicating higher absorption capacity of
Cu in vetiver root. For vetiver grown in
solutions with different Cu concentrations, the
translocation of Cu happened from the shoot
to top of vetiver. This process seems to
increase with Cu concentration in
contaminated water (Figure 4b). For other
plant species, Cu concentration at 10 mg/L in
contaminated water is toxic but vetiver can
withstand and alive at 46 mg/L.
The maximum Cu concentration in shoot,
meristematic region, and root of sample TB6
was 46.2, 119.1 and 660.7 mg/kg,
respectively, being higher than those in
previous reports (Truong and Baker, 1998,
2000; Truong and Hart, 2001; Yahua et al.,
2004; Baker, 1976). In the contaminated
water, Cu and Al concentrations were high,
their antagonisms lead to reduce uptake
capacity of Cu by roots under high Al
concentration (Kabata and Pendias, 2001).
3.3. Lead (Pb)
Pb is an essential element for the plant at
the concentration from 2 to 6 g/kg (Broyer et
al., 1972). Pb has been widely considered as a
major pollutant in the environment and a toxic
element to plants (Kabata and Pendias, 2001).
Chemical fingerprint: Pb was concentrated
in the roots of vetiver and deviation in
comparison with “reference plant” ranged
from 70.6 (BL1-R) to 130% (TB6-R) (Table
4; Figure 3). For the meristematic regions, the
deviation was lower than zero, being -100%
(TB10-R). The concentration of Pb in shoots
followed in order: (S2, S3)>S1, M, R and
increased follow its concentration in
contaminated water and was four times higher
than that in “reference plant”.
For other plants, the translocation of Pb
from root to top is greatly limited, being only
3% (Zimdahl, 1975). The translocation of
vetiver ranged from 23 to 41%.
The trend of slope line is clearly shown in
Figure 4c, Pb concentration markedly
increased with its concentration in
contaminated water. The stimulating effect of
Pb on Cd uptake by root could be an effect of
the disturbance of the transmembrane
transport of ions (Kabata and Pendias, 2001).
3.4. Tin (Sn)
Tin is very toxic to both higher plants and
fungi (Kabata-Pendias Alina and Pendias
Henryk. 2001).
Chemical fingerprint: The deviation of Sn
in vetiver in comparison to “reference plant”
was slightly lower than zero for the lower part
of TB10 (R, M and S1) and up to 142% for
the upper parts (S2, S3). The Sn concentration
in vetiver increased with its concentration in
contaminated water (TB6) and increased in all
parts of vetiver to 207% (Table 4; Figure 3).
In the shoots of vetiver grown in TB10, TB6,
Sn concentration was higher than in the root
and meristematic region by the following
order: S3, S2>S1>M, R (Figure 4d).
Unlike to other plants, most Sn
concentration remained in roots (Rommey et
al., 1975), the vetiver tends to uptake and
accumulated Zn in the upper parts, thus ratio
shoot: root varied from 82% (TB6-S1) to
277% (top of vetiver TB6-S3), and being
higher concentration in top by order
S3/R>S2/R>S1/R.
Vietnam Journal of Earth Sciences, 38(3), 286-296
294
3.5. Zinc (Zn)
Zn plays as an active enzyme, regulates
sugar consumption in plants (W. H.
Schlesinger, 2004), and involves
incarbohydrate and protein metabolism
processes (Kabata and Pendias, 2001).
Soluble forms of Zn were available to vetiver
and the uptake of Zn from soils to be linear
with its concentration in contaminated water
(Figure 4e).
Figure 4. Relationship between the concentrations of metals (Al, Cu, Pb, Sn, and Zn) in several parts of vetiver and
contaminated water
Chemical fingerprint: The deviation of Zn
concentration in meristematic regions was all
positive in comparison to the “reference
plant”, ranging from 508 - 574%, but for root
and shoot parts the deviation of Zn was
slightly >0 (Table 4; Figure 3).
N.T. Minh, et al./Vietnam Journal of Earth Sciences 38 (2016)
295
Zn concentration was higher in the
meristematic region than that in root. Roots
and meristematic regions accumulated Zn
higher than shoots, thus, the ratio shoot: root
ranged from 30 to 46%. This pattern indicated
that Zn could be translocated from the roots to
shoots of vetiver. Vetiver has higher tolerance
to Zn and Pb than other species (Yang et al.,
2003). The Zn-Pb antagonism adversely
affects the translocation of each element from
root to shoot (Kabata and Pendias, 2001).
4. Conclusions
The present study showed that vetiver
could highly accumulate metals Al, Cu, Pb,
Sn and Zn in the upper part of the shoot. Thus,
the vetiver may serve as an important means
for waste water treatment.
The roots and upper parts of shoots
accumulated Al concentration from 17-30
times and 1.2 times higher than “reference
plant”, respectively. Thus, vetiver can be
considered as Al-hyperaccumulation. In other
plants, the excessive or toxic concentration of
Cu is 20-100 mg/kg, but in vetiver plant, it
was much higher and reached up to 660 and
46.2 mg/kg in the roots and shoots,
respectively. Vetiver could withstand and
alive at the Cu concentration of 46 mg/L in
contaminated water. The Pb translocation rate
from root to shoot was up to 41%. Sn highly
accumulated in upper parts with ratio shoot:
root varied from 82 - 277% in the top and
increased to the top by order
S3/R>S2/R>S1/R. Zn could be translocated
from roots and accumulated in the shoots of
vetiver, the ratio shoot to root was up
to 46%.
Acknowledgements
We thank two anonymous reviewers for
their critical comments that significantly
improved this manuscript from an early
version. We thank the Korea Science and
Engineering Foundation, and we thank Prof.
Truong Paul, The Vetiver Network, for
providing the vetiver seedlings.
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