Introduction

The badland soil that is derived from mudrock (a class of fine-grained siliciclastic sedimentary rock) is unfavourable for plant growth because of its high clay and calcium carbonate contents1. One of the common physiochemical properties of the badland soil is the low water infiltration, thus, most rainfalls on badland fields drain via surface runoff, leading to soil erosion and nutrient loss2. Moreover, in badland soils, sodium and chlorine have been found to concentrate near soil surface during the dry season, which creates repulsive forces among soil particles, causing the soil to become rock-hard. On the other hand, during the rainy season, soils swell and soften upon water saturation, which has been shown to accelerate surface erosion3. Concentrated sodium and chlorine in this type of soil also increase soil electric conductivity, rendering it inhospitable to plant growth, resulting in bare landscapes in most badland ecosystems.

In Southern Taiwan, Plio-Pleistocene badland soils, consisting of up to 90% silt and clay combined, occupy more than 10,000 ha and are devoid of vegetation1. Soil crusting is common on the surface of this badland soil, which increases its bulk density and penetration resistance. Previous research4 has indicated that root growth could be inhibited when penetration resistance exceeds 14 kg cm−2, where the penetration resistance of the bare soil in the badlands of Southern Taiwan has been shown to be high (14.5 ± 1.47 kg cm−2)5.

Thorny bamboo (Bambusa stenostachya), a dense clumping bamboo with an average height of 12–15 m, is one of the only plant species that are able to grow in these uninhabitable soils. Research has shown that bamboo plants absorb nutrients from deep soils and retain soil water in infertile environments, as they are known to have deeper rhizomes and roots than many other non-woody plants6. A previous study reported that the ecological parameters of a highly degraded soil in India were significantly improved as a result of the increase in soil organic matter (SOM) by planting bamboos7.

Soil organic matter consists of different C fractions such as soluble, acid hydrolysable and recalcitrant C. In addition to the overall SOM pools increased by bamboo plantations, humification and the composition of SOM may be a good reflection of the impact of the plant on SOM8. During humification, organic compounds in plant litter could be transformed into humic substances, whereupon their structures become significantly altered compared to the original forms in plant materials9. To the best of our knowledge, the mechanisms by which thorny bamboo grows in badland ecosystems, and the interactions between the growth of the bamboo, soil nutrients, and microorganisms in this hostile soil environment are still not well understood. Thus, the objective of the study was to find out the difference in physical, chemical, and biological parameters of soil between bamboo plantations and adjacent bare lands in Southern Taiwan. We hypothesized that the presence of bamboo in these soils would result in significant increases in SOM and soil nutrients, and that the increase in SOM would improve soil physiochemical properties and increase soil microbial biomass.

Results

The analysis of soil properties from the three sampling locations is shown in Table 1. Soils were mostly loam to clay loam, containing high silt and/or clay content. Soil was slightly alkaline (pH = 8.3) at all locations except at the bamboo plantation in Site 2, where the soil was slightly acidic (pH = 6.2). Generally, the soil was distinctively different between bamboo plantations and bare land soils. Soil electric conductivity was significantly lower in bamboo plantation soils (0.7 mS cm−1) than in bare land soils (11.2 mS cm−1) (p < 0.05), and soil water content was higher at bamboo plantations than in bare land soils (p < 0.05).

Table 1 Soil properties (0–10 cm) under three thorny bamboo plantations and adjacent bare lands in Southern Taiwan.
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The soluble organic carbon (SbOC) content, measured using potassium chloride (KCl) extracts (SbOCKCl), was much higher at bamboo plantations than in bare land soils (p < 0.05) (Table 2). Site 2 had the highest SbOCKCl among the bamboo plantations, which was more than 2 times higher compared to bare land soil (p < 0.05). A similar trend was observed for SbOC using the hot water extraction method (SbOCHW). The mean SbOCHW was nearly 6 times higher in bamboo plantation soils than bare land soils (p < 0.05), while the highest SbOCHW was measured in the bamboo plantation soil from Site 2 (Table 3). The SbOC values from all locations were higher from samples extracted using the hot water method compared to samples extracted using KCl. The bare land soils from the three sampling locations had similar levels of SbOC, irrespective of the extraction method used.

Table 2 Concentrations of soluble N and soluble organic C in 2 M KCl extracts, SbON/TN ratio, and SbOC/TOC ratio in the top 10 cm of soil from thorny bamboo plantations and adjacent bare land in Southern Taiwan.
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Table 3 Concentrations of soluble N and soluble organic C in hot water extracts, SbON/TN ratio, and SbOC/TOC ratio in the top 10 cm of soil from thorny bamboo plantations and adjacent bare land in Southern Taiwan.
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The difference in extractable nitrogen (N) between bamboo plantations and bare land soils depended on N species. The concentrations of KCl-extracted NH4+ (NH4+KCl) and total dissolved nitrogen (TDNKCl) at the three sites were 2–4 times higher at bamboo plantations than in bare land soils (p < 0.05), whereas, KCl-extracted NO3− (NO3−KCl) and soluble organic nitrogen (SbONKCl) were similar between bamboo plantations and bare land soils. Similarly, the concentration of NH4+HW and TDNHW were 3–10 times higher in bamboo plantation soils than in bare land soils (p < 0.05), whereas NO3−HW and SbONHW were not significantly different between bamboo plantations and bare land soils, with the exception of SbONHW from Site 2, where NO3−HW and SbONHW were higher in bamboo plantation soils than bare land soils. The SbOCHW to total organic carbon (TOC) ratio (SbOCHW/TOC) was found to be higher in bamboo plantation soils than in bare land soils, however, the opposite trend was observed for SbOCKCl/TOC. No differences in the SbONHW or SbONKCl to total nitrogen (TN) ratios (SbONHW/TN or SbONKCl/TN) were observed between bamboo plantations and bare land soils.

Soil microbial biomass C (Cmic) and N (Nmic) were found to be 7–10 times higher in bamboo plantation soils than in bare land soils (p < 0.05) (Table 4). Soil respiration rates and potentially mineralisable N were also higher at bamboo plantations than in bare land soils. The amount of total mineralisable N was almost negligible in bare land soils, although a slight respiration rate was detected. The Cmic/TOC and Nmic/TN ratios were higher at bamboo plantations than in bare land soils (p < 0.05), whereas respiration/Cmic was higher in bare land soils than in bamboo plantation soils (p < 0.05).

Table 4 Soil microbial biomass, potentially mineralisable nitrogen, and microbial quotient in soils from thorny bamboo plantations and adjacent bare lands in Southern Taiwan.
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The SbOCKCl and SbOCHW in both bamboo plantations and bare land soils were significantly correlated with TOC and Cmic, respectively (Fig. 1). However, values for SbOCKCl and SbOCHW in the bare land soils were clustered and showed less dependence on TOC or Cmic. In this study SbOCHW was more strongly correlated with both TOC and Cmic than SbOCKCl, indicating that SbOCHW could be a better reflection of the effects of bamboo on soil TOC and Cmic than SbOCKCl. The overall SbONHW was significantly correlated with both TN and Nmic but not with SbONKCl (Fig. 2). The strong correlations between SbOCHW and TOC, as well as SbONHW and TN, imply that hot water may help to release more organic substrates from the soils.

Figure 1
figure 1

Relationship between soil soluble organic carbon in 2 M KCl extracts (SbOCKCl) and soil total organic carbon (a) and that between hot water extracts (SbOCHW) and soil microbial biomass carbon (b) in thorny bamboo plantations and adjacent bare lands.

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Figure 2
figure 2

Relationship between soil soluble organic nitrogen in 2 M KCl extracts (SbONKCl) and soil total organic nitrogen (a) and that between hot water extracts (SbONHW) and soil microbial biomass nitrogen (b) in thorny bamboo plantations and adjacent bare lands.

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The ∆logK (logarithmic ratio of light absorbance of humic acids at 400 and 600 nm; ∆logK = log(A400/A600)) values observed in soils from thorny bamboo plantations were significantly higher than those of bare land soils (Table 5). The contents of soil acid-hydrolysable C pool I (soil organic C extracted with 5 N H2SO4; AHPI-C), acid-hydrolysable C pool II (soil organic C extracted with 26 N H2SO4; AHPII-C), and recalcitrant C pool (residue after acid-hydrolysis; RP-C) were significantly higher in soils from thorny bamboo plantations compared to those of bare land soils. Considering that the TOC contents differed between the two types of soils, the ratios of acid-hydrolysable and recalcitrant contents to TOC were calculated. The ratios of AHPI-C and AHPII-C to TOC (AHPI-C/TOC and AHPII-C/TOC) were higher in bamboo plantation soils, while the ratio of RP-C to total organic C (RP-C/TOC) was higher in bare land soils.

Table 5 The degree of humification as indicated by ∆logK, acid-hydrolysable pool I (AHPI-C) and II carbon (AHPII-C), recalcitrant pool carbon (RP-C), and ratios of labile and recalcitrant carbon to total organic carbon (TOC) of soils from three thorny bamboo plantations and adjacent bare lands in Southern Taiwan.
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Discussion

In this study, we compared physicochemical properties of bare land soils and those planted with thorny bamboo. The data from this study shows significantly higher soil Cmic, Nmic, respiration rates, total mineralisable N, SbOCHW/TOC, and Cmic/TOC in soils from the bamboo plantations compared to bare land soils, mostly due to fast growth and high biomass production of bamboos10,11. In the present study, thorny bamboo resulted in an increase in TOC content, which also improved the labile SOM (i.e. SbOC) of the previously bare lands. For both KCl and hot water extraction methods, SbOC was 2–7 times higher in soils from bamboo plantations compared to soils from the adjacent bare lands, indicating the strong contribution of thorny bamboo growth to soil C pools.

Soil organic matter is one of the most important indicators of soil quality12, as it improves soil physicochemical properties (e.g. decreasing soil bulk density and increasing soil porosity), and increases soil water content as a result high water holding capacity of SOM13,14. These benefits provided by SOM may explain the overall improvement of soils at bamboo plantations in the present study, where soil bulk density decreased by ~30% and soil water content increased by 10%. Moreover, the highest TOC in the bamboo plantation from Site 2 helped to improve the soil quality to the extent that Site 2 was observed to have the lowest bulk density and the highest water content of all the sites in the present study.

The higher SbOCHW/TOC observed in bamboo plantation soils suggested that the observed SOM changes in bamboo plantation soils was not only in the total C pool as a result of litter from the bamboo plants, but also labile fractions as a result of bamboo litter decomposition. The lower SbOCKCl and SbOCHW of bamboo plantation soils in the current study than those in a previous study conducted in a mountainous area of Central Taiwan15 could be due to the fact that soils in the Central Taiwan contained higher TOC. In addition, the considerable lower SbOC/TOC from both KCl and hot water extractions of bamboo plantation soils in the current study than those in a mountainous area of Central Taiwan15 implys that most of the TOC in badland soils was strongly bound to the soil particles as a result of the high silt and clay contents.

The organic materials and dense roots provided by bamboo have shown to reduce overland flow velocity and infiltration rates16,17, thereby reducing soil erosion18. The export of nutrients associated with sediment loss was found to decrease as a result of bamboo plantations19, resulting in an overall accumulation of soil nutrients in bamboo plantations, as well as an improvement in soil quality20. The fact that the NH4+, SbON, and TDN measured in bamboo plantation soils in the current study were distinctively higher in comparison to bare land soils may be due to the less soil erosion in bamboo plantation soils.

The Nmic was found to be positively correlated with TN, as soils with higher levels of N support higher microbial biomass21. The higher Nmic/TN ratios at the bamboo plantations in this study indicate that bamboo plantations may have a higher capacity for N retention through the synthesis of N in microbial biomass. Potentially mineralisable N has been considered an active fraction of soil organic N22. Thus, the high potentially mineralisable N in the bamboo plantation soils in our study implies that the bamboo plantations contained high levels of active soil organic N.

Labile SOM (SbOC and SbON) are the most readily available energy source for soil microbial growth23. In the present study, SbOC was positively correlated with Cmic in bamboo plantation soils. The positive relationships between SbOC, TOC, and Cmic implies that SbOC may be derived from the decomposition of soil TOC as a result of microbial activity24. The increase in Cmic, owing to the readily available energy in SbOC, was found to increase the soil respiration rates of bamboo plantation soils. Moreover, higher Cmic/TOC and SbOCHW/TOC ratios indicate that the available organic substrates were used more efficiently by microbes in soils planted with bamboos25.

The respiration/Cmic ratio has been used in microbial studies to indicate the ecological efficiency (i.e. energy required to support the metabolism of per unit Cmic in soil) of soil microbial communities26,27. A high respiration/Cmic ratio indicates the inefficient use of energy, while a low respiration/Cmic ratio indicates high efficiency, and that higher quantities of C are utilized for biomass production26,28,29. In the present study, soil respiration appeared to be higher in bamboo plantation soils than in bare land soils. However, the respiration/Cmic ratio showed a reverse trend, and was significantly lower in soils planted with bamboo than in bare land soils (p < 0.05). This result implies that the lower respiration/Cmic ratio of bamboo plantation soils could be attributed to high microbial biomass rather than microbial activity. Moreover, the higher respiration/Cmic ratio could be a good indicator that microbes were under greater stress in bare land soils.

The value of ∆logK is a soil index to evaluate the humification status of SOM, and it generally decreases with increasing SOM humification. The lower ∆logK values observed in bare land soils indicate a high degree of humification, as there is little input of fresh litter into the soil. The growth of bamboo adds fresh litter to soils and causes the accumulation of SOM30,31. Wang, et al.32 noted that bamboo litter contains a high portion of O-alkyl-C, a C functional group that can be easily decomposed by soil microbes, which is thought to contribute to increases in the labile organic C of soils. The high AHPI-C/TOC and AHPII-C/TOC ratios of soils planted with bamboo support the notion that the decomposition of bamboo litter increases acid-hydrolysable C pools. The acid-hydrolysable C pool is small in size and has a rapid turnover, which responds rapidly to changes in C supply and affects microbial activity33,34. The higher quantity of acid-hydrolysable C pools in bamboo plantation soils could be one of indicators of their high soil quality. The high RP-C/TOC ratio of bare land soils indicates that the C of the SOM composition is relatively more recalcitrant (i.e. high molecular weight C, irregular structure, and long turnover), and therefore has a higher resistance to chemical degradation and decomposability35.

In addition, the fact that the acid-hydrolysable C and SbOC displayed similar trends between the sampling sites implies that both methods extracted similar C pools36. The observation that acid-hydrolysable C was 10–20 times higher than SbOC at all sites may be due to the fact that acid-hydrolysable C contained more slow-turnover C than hot water- or KCl-extracted C37. Hot water-extracted soil organic C has been typically considered to be readily metabolisable38, while acid-hydrolysable C has been shown to be composed of bioreactive C in soil, even if it is not readily used by microbes39. Therefore, acid-hydrolysable C is less sensitive to environmental changes, while both acid-hydrolysable C and SbOC represent the labile fractions of soil C pools36.

In conclusion, this study demonstrates that planting of thorny bamboos in uninhabitable badland soils appears to be a successful practice for soil amelioration. The thorny bamboo helped to increase SOM and improve soil physiochemical properties that contribute to soil improvement.

Methods

Site and soil sampling

This study was carried out at three locations in southwestern Taiwan—Site 1 at Zuozhen, Tainan (120°26′E, 23°0′N), Site 2 at Longqi, Tainan (120°23′ E, 22°54′N), and Site 3 at Tianliao, Kaohsiung (120°24′E, 25°51′N)—with an average altitude of 100–300 m (Fig. 3).

Figure 3: Map of soil sampling locations in Southern Taiwan.
figure 3

Elevation data used to create Fig. 3 was obtained using the Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) digital elevation model (DEM) at a resolution of 30 m ( https://asterweb.jpl.nasa.gov/gdem.asp), while contour lines were created using the ArcGIS v.10.0 software package (ESRI [ http://www.esri.com/], Redlands, CA, USA). (Triangles: thorny bamboo sites; circles: bare land sites).

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The lands chosen as sampling locations for this study are owned by the Forestry Bureau and accessed for public. Research proposals were approved and granted by the Ministry of Science and Technology, Taiwan. Field and laboratory studies did not involve any animal husbandry, nor any protected or endangered biological species.

At each site, it involved badland soils with and without bamboos. In badland, desiccation cracks occur on the slope surfaces extending to a few centimeters in the dry season. During the rainy season, the soil expands and closes the cracks to form crusts in 1–2 cm thick3. Soils in the three studied locations have high clay and silt contents (clay: 27–44%; slit: 31–47%), primarily inherited from the parent mudrock. Based on U.S. Soil Taxonomy40, soils in the badland lacking of vegetation were classified as Typic Eutrustepts, and those with the bamboo as Typic Dystrudepts. Thorny bamboo, which was cultivated in the early 1900s41 by local residents for bamboo shoots and stems, is the predominant plant on the north-facing sides of hogbacks (ridges with a sharp summit and steeply sloping sides) (Fig. 4). The south-facing sides of hogbacks are composed of bare land soils with no plant coverage. Interestingly, the downstream valley near these badlands (only a few km away) are well cultivated as orchards with various fruit trees, such as mango, jujube, and banana, indicating that original mudstone soils can be ameliorated for agricultural uses after certain improvements. At each site, three transects (replications), 50 m apart, were demarcated at both north-facing and south-facing sides of the hogbacks. Thus, there were a total of 18 transects (composited samples) for the study (2 vegetation types: bamboo and bare land soil × 3 replications × 3 locations for each soil type). A soil sample, composited of 8 soil cores, was collected in each transect by a soil auger (4.25 cm in diameter) and stored in plastic bag. The collected soil samples were stored at 4 °C until laboratory analysis.

Figure 4: Landscape of mudstone badlands at Zuozhen in Tainan City, Southern Taiwan.
figure 4

South-facing slopes are barren while north-facing slopes are covered with thorny bamboo (photo by CYC, corresponding author).

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Laboratory analyses

General properties of soil

Soil pH was measured in a 1:1 soil to water suspension using a portable Jenco 6009 pH/mV meter. Soil electrical conductivity was measured using a saturated extract method42. Soil total organic carbon (TOC) was analysed using a Fisons NA1500 elemental analyser (ThermoQuest Italia, Milan, Italy) after removing carbonate with 1 N HCl. Briefly, 0.3 g of soil was weighted out, mixed with 0.5 ml of HCl and air dried for 12 h before analysing with the elemental analyser. Soil TN was determined using the Kjeldahl digestion method43. Deionized water was added to the digested solution to a volume of 100 ml and analysed using the previously described indophenol method44 and measured spectrophotometrically (UV-1201, Shimadzu Corp., Kyoto, Japan). To determine the soil water content, soil was oven dried at 105 °C for 24 h and weighed for water loss. Soil texture was determined using the hydrometer method45. Soil bulk density was determined using the weight and volume of soil samples collected via cores.

Soil extractable nutrients

Soil nutrient contents, including NH4+, NO3−, SbON, and SbOC, were measured using two different extraction methods, KCl extraction and hot water extraction, described in Chen et al.46 with modification. For the KCl extraction, 5 g of air-dried soil from each replicate sample was weighted out, placed in a 250-ml conical flask, and injected with 50 ml of 2 M KCl. The flask was sealed with plastic paraffin film and shaken for 60 min at 150 rpm. The solution was collected by filtering the slurry using filter paper (Whatman No. 5).

For the hot water extraction method, 6 g of air-dried soil samples were weighed, placed in a 50-ml centrifuge bottle, and injected with 30 ml of distilled deionized water. The bottle was placed in an 80 °C water bath and incubated for 18 h, subsequently shaken for 5 min at 150 rpm, and the solution was collected by filtering the slurry using the same size filter paper as KCl extracts. Extracted NH4+ was analysed using the indophenol method with a spectrophotometer at 635 nm wavelength (UV-1201, Shimadzu Corp., Kyoto, Japan). The NO3− was determined using the cadmium reduction method47 with a flow injection analyser (SP-8001, Metertech Inc., Taipei City, Taiwan). Soil TDN was digested to NO3− using the persulfate method48 and was then analysed as aforementioned with a flow injection analyser. The SbON was calculated by subtracting NO3− and NH4+ from TDN. The SbOC was measured using a TOC analyser (1010, O.I. Analytical, Texas, USA).

Soil microbial biomass C and N

Soil Cmic and Nmic were analysed using a chloroform-fumigated extraction method49. Briefly, four 10 g aliquots of soil were weighed out from each sample and placed in a 250-ml conical flask. Then, soil samples were equally separated into two sets of 36 samples. One set of soil samples were fumigated using chloroform for 24 hours and extracted with 50 ml of potassium sulphate (0.5 M K2SO4). The other set of soil samples were directly extracted with 50 ml of K2SO4 (0.5 M). The C in K2SO4 solutions was determined using a TOC analyser and N was analysed using a previously described protocol50. The Cmic and Nmic were calculated as the differences between the fumigated and unfumigated K2SO4-extractable C and N by multiplying coefficients (KEC = 2.22 and KEN = 4.95) [(fumigated C (N) − unfumigated C (N)) × coefficients]51,52.

Soil respiration

Soil respiration rate was estimated from the total amount of CO2-C during a 3-day incubation using an alkali method15,53. Briefly, 20 ml of 0.05 M NaOH was injected into a 250-ml flask and a plastic tube and 20 g of fresh soil sample was placed in the flask. After 3 days of incubation at 25 °C, the 20 ml NaOH solution was titrated using 0.05 M HCl with phenolphthalein and BaCl2.

Total mineralisable N

Total mineralisable N was determined using the waterlogging incubation method54. Briefly, 5 g of moist field soil was weighed out from each sample, placed in a 250-ml centrifuge bottle with 25 ml of distilled deionized water, and incubated and shaken in an incubator at 40 °C for 7 d. After incubation, 25 ml of 4 M KCl was injected into the centrifuge bottle and shaken for 1 h at 150 rpm. Subsequently, the bottle was centrifuged at 2000 rpm for 20 min and 50 ml of water was extracted and filtered for the determination of NH4+ concentration.

Extraction of humic acids for photometric analysis

One gram of air-dried soil from each sample was weighed and shaken at 150 rpm with 30 ml of 0.1 N NaOH at 100 °C for 30 min. The Na2SO4 (2 ml) was added and the samples were subsequently centrifuged at 10,000 × g for 15 min. Precipitates were further extracted with a mixed solution of 20 ml of 0.1 N NaOH and 3% Na2SO4, and centrifuged at 10,000 × g for 15 min, twice. The extractant was quantified to 100 ml with deionized water and then acidified with 1 ml concentrated H2SO4 (98%). Precipitates were subsequently dissolved in 30 ml of 0.01 N NaOH to determine the ratio of humic acids9 using a spectrophotometer (Hitachi U-2000). The light absorbance of humic acids was measured at 400 and 600 nm to determine their molecular fractions, as the smaller fractions of humic substrates tend to absorb shorter wavelengths of light55. The degree of humification was determined by calculating the ∆logK value, which is the logarithmic ratio of the absorbance at 400 and 600 nm (∆logK = log(A400/A600))56. The ∆logK is an inverse index of the condensation of the aromatic network in the macromolecules of humic acids, representing the degree of humification.

Determination of acid-hydrolysable and recalcitrant C

Acid hydrolysis is a chemical fractionation method used to separate acid-hydrolysable SOM and recalcitrant SOM pools (unhydrolysable)33. The two-step acid hydrolysis is used to isolate and quantify labile and recalcitrant substances of SOM with sulphuric acid (H2SO4) as the extractant57. Briefly, 0.5 g of each soil sample was hydrolysed with 20 ml of 5 N H2SO4 at 105 °C for 30 min in Pyrex flasks with Allihn condensers. Samples were centrifuged at 20,000 × g for 10 min and decanted to collect the hydrolysable SOM from each sample. Residues were flushed with 20 ml of deionized water, and the extract was added to the previous hydrolysate. The C from the hydrolysate was regarded as the AHPI-C. The remaining residual SOM was hydrolysed with 2 ml of 26 N H2SO4 overnight while shaking continuously at room temperature. The concentration of H2SO4 in the sample was brought down to 2 N by dilution and hydrolysed for 3 h by heating at 105 °C. The resulting hydrolysate was considered as AHPII-C. The remaining SOM in the sample, regarded as RP-C, was flushed with 30 ml of deionized water and dried at 60 °C in a pre-weighed crucible. AHPI-C and AHPII-C were measured using a TOC analyser (1010, O.I. Analytical, Texas), while the RP-C was determined by an NSC elemental analyser (Fisons NA1500).

All analyses in the study were performed in duplicate. All results have been converted on dry weight basis.

Statistical analyses

Differences in soil nutrients between bare lands and bamboo plantations at all locations were tested for significance using a one-way analysis of variance (one-way ANOVA). When the one-way ANOVA revealed interactions between sites and soil physicochemical properties, Tukey’s honestly significant difference (HSD) test was applied to further test the means of all pairs of dependent variables. Relationships between two soil properties were analysed using bivariate regression analysis. All statistical analyses were performed using JMP (Version Pro 10, SAS Institute, Cary, NC, USA). The level of significance was set at 0.05 for all tests.

Additional Information

How to cite this article: Shiau, Y.-J. et al. Improvement in the biochemical and chemical properties of badland soils by thorny bamboo. Sci. Rep. 7, 40561; doi: 10.1038/srep40561 (2017).

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