Insight into the Adaptability of Dominant Plant <i>Indigofera amblyantha</i> Craib for Ecological Restoration of Rock Slopes in Stone Coal Mine

Peng, Lu; Mao, Qiming; Cao, Lin-Ying; Sun, Hailong; Xie, Xiande; Luo, Shuang

doi:https://doi.org/10.1155/2021/3827991

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Abstract Introduction Materials and Methods Discussion Conclusions Data Availability Conflicts of Interest Acknowledgments Supplementary Materials References Copyright Related Articles

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Biogeochemical Processes, Interactions, and Control of Pollutants in Soil-Plant Systems

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Volume 2021 | Article ID 3827991 | https://doi.org/10.1155/2021/3827991

Insight into the Adaptability of Dominant Plant Indigofera amblyantha Craib for Ecological Restoration of Rock Slopes in Stone Coal Mine

Lu Peng,^1,2Qiming Mao,¹Lin-Ying Cao,¹Hailong Sun,³Xiande Xie,¹and Shuang Luo¹

Academic Editor: Hai-Bo Qin

Received10 Sept 2021

Revised07 Oct 2021

Accepted08 Oct 2021

Published01 Nov 2021

Abstract

The eco-restoration was a very effective measure to solve the problem of environmental pollution caused by the exposed mine surface in the stone coal mine site. In this study, the dominant plant, Indigofera amblyantha Craib, was well adapted to the eco-restoration in stone coal mining area. The changes of nutrient elements, pH, heavy metals in substrate material, the biological concentration/transfer factor, and the distribution and diversity of bacteria and fungi in rhizosphere soil were investigated. The results show that the plant communities help slow down the loss of nutrient elements and the increase of the concentrations of heavy metals in the eco-restoration process. The Indigofera amblyantha Craib had the advantaged ability to enrich and transfer Cd, Cu, Mn, and its diversity index of microbial communities in rhizosphere soils was higher than that of other quadrats. These excellent properties found in this work help reveal the insight into the adaptability of Indigofera amblyantha Craib in the eco-restoration of stone coal mines. It is valuable to evaluate Indigofera amblyantha Craib for eco-restoration engineering of stone coal mine and extend the application in heavy metal contaminated sites.

1. Introduction

Stone coal is a kind of combustible with the characteristics of low-carbon, low-calorific, high-ash, and high-sulfur [1, 2]. The constituents of stone coal are complex associated with polymetallic composition [3, 4]. Thus, stone coal is an important resource of vanadium (V) [2]. More than 87 wt.% of the domestic reserve of V came from stone coal in China [5]. V has been widely used in chemical industries, metallurgy, atomic energy, aviation, and so on [6–8]. Then, the increasing demand for V led to the intensification of the exploitation of stone coal mines [9, 10], which formed a lot of bare slopes and waste piles exposed to the air. The acidic mine discharge (AMD) was formed when these bare minerals oxidized by oxygen and came into contact with the rainwater [11, 12]. The AMD could future dissolve some heavy metals discharged into water [13, 14]. The leaching concentration of heavy metals from stone coal was largely dependent on solution pH [15], the 10.41% Cd, and 0.07% Pb could be released from stone coal over 7 days in pH 3.5 [16]. For the fine particle sizes of stone coal, the dissolved rates of Pb, As, Cd, and V were 0.95%, 2.96%, 0.25%, and 0.35% after 100 days in pH 4.5 solution, respectively [17]. These heavy metals further hazarded surrounding farmland and rivers, which caused the environmental situation of sites around stone coal wastes was not optimistic [18]. Thus, it was an urgent need to solve the problem of environmental pollution in the stone coal mine site.

The eco-restoration was a very effective measure to prevent AMD formation and to green the exposed mine surface [19–21]. However, due to lack of the conditions of water, nutrients, and soil layer for plant growth, and with the extreme microclimatic, edaphic conditions, and heavy metals pollution, it was difficult for eco-restoration of exposed rocky slope in the stone coal mine [21–27]. Cutting and sorting slopes, covering soil, and planting plants were the main methods at present [28–30]. The growth status of plants was an important criterion for measuring ecological restoration. Thus, selecting tolerant plant species was essential to ecological restoration. For example, Cynodon Dactylon (L.) Pers., Paspalum paspaloides, and Zoysia japonica Steud are used in slope vegetation restoration in East China. Robinia pseudoacacia L. and Indigofera amblyantha Craib were used in the slope of roads and railways for ecological restoration [31, 32]. These plants had the characteristics of strong drought tolerance and resistance to infertility. In addition, Indigofera amblyantha Craib was used in the tungsten mine site for ecological restoration [33] and was found that had the moderate tolerance and bioaccumulation capability for Pb and Cd [34, 35]. However, the drought, loss of nutrients, and heavy metal stress were the important limiting factors on these sites for plant establishment [36]. But there were still plants that can grow tenaciously in extreme environments. Therefore, these plants had unique adaptability to unfavorable environments.

In this study, we firstly found that Indigofera amblyantha Craib grow well in stone coal mine slope after artificial eco-restoration and was the dominant plant in all shrubs. However, there was a lack of research on the adaptation of Indigofera amblyantha Craib to heavy metal contaminated sites and its tolerance to heavy metals. Therefore, the growth of Indigofera amblyantha Craib was closely related to the effect factors and the distribution of heavy metals in soil, which help understand the adaptability of Indigofera amblyantha Craib. As a result, these findings help guide the eco-restoration engineering of the stone coal mine.

2. Materials and Methods

2.1. Study Sites and Ecological Engineering

The site of ecological restoration engineering of stone coal mine was in Nijiang Kou, Yiyang City, Hunan province. The area belongs to the subtropical humid continental monsoon climate. The total area of the ecological restoration engineering was about 75,000 m², and the construction was completed in March 2019. In this study, the representative area of 3,000 m² was selected as the study area to future analyze the changes in the recovery process.

The ecological restoration engineering was adopted the thick layer substrate material spraying after hanging net for vegetation restoration [37]. The ecological engineering is carried out sequentially in accordance with the process of galvanized wire mesh fastened, herbaceous fibers added to mesh, substrate material and seeds sprayed, and nonwoven fabric covered. A detailed description of the ecological restoration engineering was shown in Text S1 Supplementary Information (SI).

2.2. Materials Used in Ecological Engineering

The substrate material was composed of a variety of material mixing, including soil, peat soil, sawdust, organic fertilizer, compound fertilizer, aggregate agent, water retention agent, biobacterial manure, and seed according to a certain proportion (Table S1). The soil was sticky laterite (, ) without stones or gravel. The peat soil and sawdust were used to improve the soil structure and increase the content of organic matter, water conservation, and prevent loss. The organic fertilizer is the product of pig manure fermentation (). The compound fertilizer could provide nitrogen, phosphorus, and potassium for plant growth (China Agricultural Materials Group, , , and ). The aggregate agent could improve soil structure and promote oxygen supply (provided by Hunan ZhiLan Ecological Environment Construction Co. Ltd.). The soil water retention agent was anionic polyacrylamide (PAM) (Shanghai Wshine Chemical Co., Ltd., Shanghai, China, particle diameter 0.02 mm, the active ingredient concentration 99.9%). The biobacterial manure could accelerate the substrate material microbial life activities and improve the transformation of nutrients and plants to absorb nutrients.

The selection of plant species was based on reports in successful engineering from common rock slope and similar mine restoration [38–40]. Table S2 listed the selected plant species and densities used well applied in rocky slopes eco-engineering.

2.3. Sample Collection and Analysis

The investigation time lasted for 2 years after eco-restoration. Twelve samples were established at four different locations in the study area to assess plant species and communities in eco-engineering restoration. The Indigofera amblyantha Craib was the dominant species in the fruticose community due to it had the highest importance value (IV) (detail see Text S2), which could reflect the position and function of a species in a given community [41]. The sampling and handing methods of substrate material and plants (root, leaf, stem xylem, stem phloem, and fruit/seed) saw Text S3.

The pH, total nitrogen (TN), total phosphorus (TP), total potassium (TK), total organic carbon (TOC), hydrolyzable nitrogen (HN), available phosphorus (AP), and available potassium (AK) of substrate material samples were analyzed. The pH was determined by the potentiometry method. The organic matter (TOC) was measured by the potassium dichromate external heating method [42], and the total phosphorus (TP) and available phosphorus (AP) were determined by alkali fusion and sodium bicarbonate extraction Mo-Sb antispectrophotometric method, respectively [43, 44]. The total nitrogen (TN) and hydrolysable nitrogen (HN) were measured by the Kjeldahl nitrogen analysis method [45] and the alkali hydrolysis diffusion method [46]. The total potassium (TK) and available potassium (AK) were determined by atomic absorption spectrometry [47] and acetic acid extraction-flame photometric method [48]. The content of heavy metals, including Pb, Cd, Cr, As, Cu, Zn, Ni, Sb, Mn, and V in stone coal, artificial soil, and plants, were measured by ICP-OES (NexION 350X, PerkinElmer, USA) after digesting tissues following the Chinese National Standards for Food Safety Determination of multiple elements (GB5009. 268-2016).

The composition of rhizosphere microorganisms also has a certain relationship with plant adaptability. For the extraction of bacteria and fungi to analyze microbial diversity, a part of substrate material sampling was stored at −20°C at the twenty-first month (2020.12) after vegetation restoration. In addition, adjacent natural environment samples were supplemented, including bamboo forests, rice paddies, river shoal sediments, grasslands, exposed ditches, and stone coal. The microbial samples were then sent to Novogene Technology Co., Ltd (Beijing, China), and sequencing was analyzed based on the Illumina NovaSeq PE250 [49]. The results of species, clustering, and diversity analysis based on operational taxonomic units (OUTs) were provided by Novogene.

A redundancy analysis (RDA) was used to find out the positive or negative effect of environmental factors on the eco-restoration diversity by adopting CANOCO 5.0 [50].

3. Result

3.1. Nutrient Elements in the Substrate Material

Soil provided a substrate for the exchange of material and energy for plant growth and played an essential role in plant growth, especially in the process of ecological restoration [51–53]. First, the pH in substrate material was a clear drop starting from to and then gradually rose to about (Figure S1). The acid wastewater leached from the stone mine slope might be the dominant reason leading to pH decline [54, 55]. Various metal sulfides in the stone coal mine were oxidized to sulfates in contact with atmospheric oxygen and rain, which caused pH to decrease in substrate material [56]. The vegetation in eco-engineering restoration prevented most oxygen from contacting sulfur compounds, which have slowed down the formation of AMD [57].

The HN, AP, and AK were significant decline trends with recovery time in the substrate material (Figure 1). The concentration of HN, AP, and AK were reduced by 63.4%, 94.8%, and 83.1%, respectively, from initiation. However, the HN and AK increased slightly in the twenty-first month. The total N, P, and K decreased by 49.7%, 73.8%, and 45.7%, respectively, from initial to the 18^th month. However, the rate of decline of TN, TP, and TK in the second year was significantly slower than that in the first year, and their concentrations began with upward trends from the 18^th to the twenty-first month. The rain and plant absorptions were the main driving factors in the decrease of HN, AP, and AK [58]. The small increase of HN and AK may be the decomposition of litterfall [59] or the degradation of slow-acting components such as organic fertilizers. It is worth noting that the TOC has been on the rise since the 6^th month. The TOC (twenty-first month) in the soil layer was 1.88 times higher than the initial content. Hu et al. and Liu et al. suggested that vegetation restoration was beneficial to increase the content of organic matter in the soil [60, 61]. The reason may be that (1) the TOC in the soil layer was easily absorbed by the soil and peat in the matrix and less loss with water [62]; (2) the organic acids secreted by plant roots were accumulated in the soil [63, 64]. It indicated that the restoration of vegetation was conducive to the increase of organic matter. The linear regression (LR) and nonlinear regression (binomial regression, BR) fitting results showed that there were significant positive correlations between HN and TN, AP and TP, and AK and TK (Figure S2). The high determination coefficients ( 0.936–0.971 for LR and 0.955–0.981 for BR, respectively) suggested that the contents between available states and total states were a close correlation, which indicated that the loss of , , and were mainly in the form of HN, AP, and AK.

3.2. Changes of Heavy Metals in the Substrate Material

Despite, the bare stone coal has been covered by a layer of artificial substrate material, but there had still heavy metals leaching from stone coal in the early stages when there was rain and oxygen [11, 56]. Thus, stone coal still was an important source of heavy metals, the concentrations of which were significantly higher than that of initial substrate material (init.), except Mn (Table S3). And the concentrations Mn were a downward trend from the initial to the 18^th month and then increased again. The possible reason was that the initial addition of quick-acting fertilizers contained high levels of Mn, but it lost heavily in early recovery time. The changing trend of heavy metals in the substrate material can be divided into 3 groups (Figure 2): (1) first rises and then fall, as Pb, Cu, Sb, and V; (2) increase overall, as Zn, Ni, and Cd; (3) increase first, then decrease, then increase, as Cr and As. The reason may be these heavy metals of group with the similar physicochemical properties and environmental behaviors in artificial soil environments. The biological concentration factor (BCF) and biological transfer factor (BTF) of heavy metals (Text S4) showed that Indigofera amblyantha Craib had a stronger ability to enrich and transfer Cd, Cu, Zn, and Mn and with a good tolerance to Pb, Sb, V, and Cr (Figure S3). After being absorbed by roots in the soil, Cd, Cu, and Mn were mainly transferred to leaves, while Zn was mainly accumulated in stem-phloem and roots. It suggested that Indigofera amblyantha Craib has a good tolerance to these heavy metals.

However, these changes of heavy metals in artificial substrate material were closely related to many factors, among them, the interaction of plants and microorganisms might be the important factor.

3.3. Microorganisms in the Substrate Material

The species distribution and diversity of bacteria and fungi were analyzed from 17 soil samples (Table S4) obtained from adjacent natural environments (R0, including bamboo forests, rice paddies, and river sediments), herbs and grasslands (R1) in eco-restoration, Indigofera amblyantha Craib rhizosphere soil (R2), other fruticose rhizosphere soil (R3), bare stone coal (R4), and gully formatted from artificial soil (R5). A total of 9801 OTUs were detected in the bacterial community, which were annotated to 82 phyla, 180 classes, 391 families, 547 orders, 905 families, 905 genera, and 1401 species. Most of them belong to Actinobacteria, Gemmatimonadetes, Acidobacteria, Proteobacteria, Chloroflexi, etc. For fungi, 2753 OTUs detected were attributed to 17 phyla, 66 classes, 172 orders, 370 families, 761 genera, and 1072 species, which mostly belong to the Ascomycota, Basidiomycota, Mortierellomycota, Chytridiomycota, etc.

In the relative abundance of the top 10 species in phylum and genus levels, there was a great difference among groups (Figure S4). Although Proteobacteria and Ascomycota occupied a significant proportion of each group of bacteria and fungi in the phylum levels, respectively, there were still differences in the distribution of species in phylum levels (Figure S4). The differences in the composition of species were especially evident at the genus level. For the eco-restoration groups (R1, R2, and R3), the rhizosphere microorganisms of different plant species were also significantly different. Combination with the heatmap analysis of bacteria and fungi species could further identify the dominant species. From the clustering heat map of bacteria and fungi at the genus level (Figure 3), there were significant differences in species clustering among groups. The species with great relative abundance were the dominant species in the groups.

(a)

(b)

For the bacteria, the abundance of Meiothermus, Occallatibacter, an uncultured Chloroflexi bacterium (named 1921-2), and Acidothermus was higher than other species in R0 group (natural environment). The Nitrosomonas, Candidatus Jettenia, and Candidatus Kuenenia were mainly species in the soil of herbs and grasslands samples (R1). The main species of bacteria in the rhizosphere soil of Indigofera amblyantha Craib samples (R2) were Gemmatimonas and Conexibacter Sphingomonas, and that of other fruticose samples (R3) were Pseudomonas, Flavobacterium, and Acidibacter. For the bare stone coal samples (R4) and exposed ditches formatted from the slope of recovered (R5), the main species were Granulicellas, Streptococcus and Acidiphilium, Ferrimicrobium, Acidithiobacillus, Acidibacter, and Sulfobacillus, respectively.

The genus classification position clustering of fungi was more obviously different than bacteria among groups (Figure 3). The species of great relative abundance of R0 group were Wickerhamiella, Piedraia, and Sarcodon, and that of R1 group were Clavaria, Capnodicles, and Curvularia. For Indigofera amblyantha Craib samples group (R2), Tricholoma, Sordariomycetes, Chaetomium, Ascomycota, Periconia, Pyronemataceae, and Tricholadium were mainly genera, and Cercospora, Nigrospora, Hypochnicium, Arcopilus, Coniochaeta, Cladosporium, Botrytis, and Pseudopithomyces were mainly genera in R3 group. The main genera of fungi in R4 and R5 were concentrated in Fusarium, Apiotrichum, Sonoraphlyctis, Zygophlyctis, and Boothiomyces and Fodinomyces, Mortierella, Talaromyces, and Humicola, respectively.

The species abundance and classification position clustering reflected the dominant species among groups but did not reveal indicate differences in community structure and diversity [65]. Therefore, the Shannon-Wiener diversity index was used to analyze intergroup diversity (Figure S5). For the bacteria, the Shannon index of eco-restoration groups (R1, R2, R3) and adjacent natural environments (R0) were obvious higher than the bare stone coal samples (R4) and ditches (R5). However, for the fungi, the Shannon index of fruticose samples (R2 and R3) was higher than in other groups. The Shannon index of fungi in R4 and R5 groups was higher than that of bacteria. This shows that different environments and plant communities have a great influence on the composition of microorganisms. It is worth noting that the Shannon indexes of bacteria and fungi in Indigofera amblyantha Craib samples (R2) were at a higher level in all groups. The Indigofera amblyantha Craib as dominant species in eco-restoration had a great promoting effect on improving soil microbial diversity.

4. Discussion

4.1. Relationship between Community and Factors

The redundancy analysis (RDA) could identify the factors that had a greater impact on the plant species [50, 66]. The longer the radiation of the environmental factor, the greater the influence of the factor. When the angle between different environmental factors and/or species was acute, it indicated a positive correlation, and on the contrary, obtuse represented a negative correlation between them [66–68]. The RDA analysis between IV of plant species and environmental factors (pH, nutrient elements, TOC, and heavy metals) is shown in Figure 4. The first two axes explained 76.4% of the microbial community variation (axis 1: 41.0%, axis 2: 35.4%). The total variation was 0.841 and . The TOC, HN, AP, Sb, Cd, and V in the substrate material were the main environmental factors affecting the IV of plant species (Figure 4). The IV of Indigofera amblyantha Craib was a positive correlation with HN, AP, V, and Sb, and a negative correlation with TOC and Cd. It suggested that Indigofera amblyantha Craib growth was less affected by other factors, and the increase of HN, AP, and Sb will facilitate its growth.

(a)

(b)

4.2. Characteristics of Indigofera amblyantha Craib

Indigofera amblyantha Craib could grow well in poor and pH 4.5-7.5 soil due to the characteristics of resistance to infertility [69, 70]. In addition, Indigofera amblyantha Craib has a strong drought tolerance [71, 72]. Under the conditions of water drought stress simulated by PEG (polyethylene glycol) solution as nutrient solution, the Indigofera amblyantha Craib seeds could germinate normally under the concentrations of 0-250 g L^–1 PEG, and with 80.2% of the normal germination rate under the simulated drought condition of 150 g L^–1 PEG [73]. The Indigofera amblyantha Craib could effectively prevent water loss and ensure its normal physiological activities under drought conditions [74]. The Indigofera amblyantha Craib also could reinforce the tensile and shear strength of roots-soil, which contributed to maintain the stability of eco-restoration in slope and prevent nutrient loss [75, 76]. The tensile strength of root was 21.15-76.08 MPa [77], and the maximum shear strength of root-soil was about 250 KPa [78]. Thus, these characteristics of Indigofera amblyantha Craib determined its dominant position under adverse circumstances.

4.3. Indigofera amblyantha Craib and Microorganism

In addition, the bacteria and fungi as the biotic factors, it also affected the community composition and the plant species growth to some extent. It could be confirmed to a certain extent from the differences in abundance and clustering of microbial species in different groups (Figure 3 and S4), and the diversity of microorganisms was higher than that of other plant species (Figure S5). The root of Indigofera amblyantha Craib could form distinct nodules with the nitrogen fixation ability (Figure S6), which provided a certain nitrogen source for plant growth. Xi et al. confirmed that there had 12 species of rhizobium associated with the roots of Indigofera amblyantha Craib in rocky desertification area, Guizhou Province, China, the dominant genus was Bradyrhizobium [79]. Yang et al. investigated the eco-restoration of quarry wastelands by planting Indigofera amblyantha Craib as the main species. The results suggested that Indigofera amblyantha Craib was beneficial to microbial diversity in soil compared with other shrub species [80]. Wu et al.’s research result showed that the arbuscular mycorrhizal (AM) fungi were easy to infect the root of Indigofera amblyantha Craib, and the infection rate reached 80.2%. The abundance of Glomus liquidambaris, Acaulospora aporocarpia, and Acaulospora scrobiculata were relatively higher [81]. The AM infection could significantly improve the uptake of phosphorus nutrients in low phosphorus soils [81]. It was worth noting that the formed AM-symbiotic structure with the ability to fixate and isolate heavy metals reduced the transport of heavy metals from roots to the ground [82]. For example, the AM reduced the transport of Zn, Cd, As, Cr, and Cu to the aboveground part of the plant [83, 84]. On the whole, the microbial communities in rhizosphere soils may be an important favorable factor contributing to their adaptability.

4.4. Tolerance of Heavy Metals

Tang et al. planted the Indigofera amblyantha Craib in the tungsten mine site for ecological restoration. Through the analysis of heavy metals in the soil, it was inferred that the absorption of Cu, Zn, and As was relatively significant [33]. Yin et al. found that the Cu content of the soil in used Indigofera amblyantha Craib eco-restoration in the abandoned quarry was lower than that of other species and suggested it had a good enrichment capacity for Cu [85]. Their findings confirmed that Indigofera amblyantha Craib had a good capacity of accumulation and transport of Cu and Zn from stone mines in this study. Chen et al. reported results suggested that Indigofera amblyantha Craib had moderate tolerance and bioaccumulation capability for Pb and Cd [34, 35]. However, there was no advantage of Indigofera amblyantha Craib on accumulative, transport, and tolerance to Pb was found in this study. Besides, there was no research related to heavy metals in Indigofera amblyantha Craib. Although Indigofera amblyantha Craib does not meet the standard of heavy metal super accumulation plant, it still can be used for the ecological restoration of soil contaminated by Cd, Cu, Zn, and Mn or mining areas due to its strong enrichment and transport capacity for Cd, Cu, Zn, and Mn and its large biomass.

5. Conclusions

In this study, Indigofera amblyantha Craib has shown great adaptability based on two years of follow-up investigation on eco-restoration engineering in expose slopes of the stone coal mines. We studied the factors related to plants growth and their influence on important values (IV) of plants used in the eco-restoration. These important factors included pH, nutrient elements (N, P, K, and TOC), heavy metals in substrate material with recovered time, and the composition of microbial communities in rhizosphere soils. The dominant species Indigofera amblyantha Craib showed a positive correlation with HN, AP, V, and Sb, and negative with TOC and Cd by the redundancy analysis (RDA). Meanwhile, Indigofera amblyantha Craib had a better ability to enrich and transfer Cd, Cu, Zn, and Mn and with a good tolerance to Pb, Sb, V, and Cr. Furthermore, the root of Indigofera amblyantha Craib could form distinct nodules, and its composition of microbial communities in rhizosphere soils was different from that of other plants. Indigofera amblyantha Craib was also beneficial to microbial diversity in soil compared with other shrub species. In addition to its drought-tolerant and barren-tolerant characteristics, these factors were helpful to explain the adaptability of Indigofera amblyantha Craib in the eco-restoration of stone coal mines. Overall, the results of this study could shed light on the applicability of Indigofera amblyantha Craib in eco-restoration engineering of mining areas.

Data Availability

All data generated or analyzed during this study are included in this article.

Conflicts of Interest

The authors declare that they have no conflicts of interest.

Acknowledgments

Funding from the Science and Technology Innovation Program of Hunan Province (2020RC2053), Hunan Provincial Key R&D (2018WK4007), the Open Fund from the State Key Laboratory of Hydraulics and Mountain River Engineering (SKHL2009), and the Double First-class construction project of Hunan Agricultural University (SYL201802005) is gratefully acknowledged.

Supplementary Materials

Supplementary Material provides the detailed description for ecological engineering, collection and preparation of samples, and analytical and calculations of data. And the Tables and Figures in Supplementary Material help to explain the content of the Manuscript. (Supplementary Materials)

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