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Research article · 2025 · Full text

International Journal of Agriculture and Nutrition

Impact of biochar application on soil physical properties and nutrient availability in sandy loam soils

Hari RanaZubin DixitDheeraj TyagiVandana Ojha

Volume 7(2) · Pages 154–156 · DOI: 10.33545/26646064.2025.v7.i2c.472 ↗

Research areasSoil Carbon and Nitrogen DynamicsAgricultural Science and FertilizationSoil Management and Crop Yield

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Abstract

Author-written

A farmer in Punjab once described his sandy loam field as "a sieve that lets water and fertiliser run straight through." This research evaluated biochar application at four rates (5-20 t ha⁻¹) on soil physical properties and nutrient availability in sandy loam at KVAU Ludhiana and NDUAT Kumarganj over 2021-2023. Biochar at 20 t ha⁻¹ increased soil organic carbon by 112%, WHC by 22.7%, CEC by 18.6%, and available N by 34.6% while reducing bulk density by 8.4%. Effects were dose-dependent and consistent across sites.

Summary

Source-checked

Plain-language reading of the full paper, prepared with AI and checked against the text. Each point links to the authors' own words.

  1. Why it matters

    • Sandy loam soils in the Indo-Gangetic Plains suffer from poor water and nutrient retention due to low organic carbon levels. View evidence ↗

      Why it matters

      Sandy loam soils in the Indo-Gangetic Plains suffer from poor water and nutrient retention due to low organic carbon levels.

      In the paper's own words

      “Sandy loam soils in the Indo-Gangetic Plains are particularly in need of these improvements because their low organic carbon results in poor water and nutrient retention”

      Page 1

      Found in: Introduction

      Read it in the full textOpen PDF at page 1 ↗
    • Biochar can improve soil because its porous structure enhances water retention and its cation exchange sites prevent nutrient leaching. View evidence ↗

      Why it matters

      Biochar can improve soil because its porous structure enhances water retention and its cation exchange sites prevent nutrient leaching.

      In the paper's own words

      “Its porous structure improves water retention, while its cation exchange sites hold nutrients against leaching”

      Page 1

      Found in: Introduction

      Read it in the full textOpen PDF at page 1 ↗
  2. The question

    • The study aimed to quantify how different doses of rice-husk biochar affect soil properties at two sandy loam sites in Punjab and Uttar Pradesh. View evidence ↗

      The question

      The study aimed to quantify how different doses of rice-husk biochar affect soil properties at two sandy loam sites in Punjab and Uttar Pradesh.

      In the paper's own words

      “This research quantified the dose-response relationship between rice-husk biochar and changes in soil properties at two representative sandy loam sites in Punjab and Uttar Pradesh”

      Page 1

      Found in: Introduction

      Read it in the full textOpen PDF at page 1 ↗
  3. What they did

    • The biochar used in the study was produced from rice husks via slow pyrolysis at 450°C for 2 hours. View evidence ↗

      What they did

      The biochar used in the study was produced from rice husks via slow pyrolysis at 450°C for 2 hours.

      In the paper's own words

      “Rice-husk biochar was produced by slow pyrolysis at 450°C for 2 hours.”

      Page 1

      Found in: Material And Methods

      Read it in the full textOpen PDF at page 1 ↗
    • Biochar particles smaller than 2 mm were incorporated into the top 15 cm of soil prior to the 2021 kharif rice season. View evidence ↗

      What they did

      Biochar particles smaller than 2 mm were incorporated into the top 15 cm of soil prior to the 2021 kharif rice season.

      In the paper's own words

      “Biochar was crushed to <2 mm and incorporated into the top 15 cm before kharif rice 2021”

      Page 1

      Found in: Material And Methods

      Read it in the full textOpen PDF at page 1 ↗
    • The researchers measured bulk density, porosity, water holding capacity (WHC), organic carbon (OC), cation exchange capacity (CEC), and available nitrogen (N) and phosphorus (P). View evidence ↗

      What they did

      The researchers measured bulk density, porosity, water holding capacity (WHC), organic carbon (OC), cation exchange capacity (CEC), and available nitrogen (N) and phosphorus (P).

      In the paper's own words

      “Bulk density, porosity, WHC, OC, CEC, available N and P by standard methods”

      Page 1

      Found in: Methods

      Read it in the full textOpen PDF at page 1 ↗
  4. What they found

    • Applying biochar at 20 t ha⁻¹ led to significant improvements: organic carbon increased by 112%, water holding capacity by 22.7%, CEC by 18.6%, and available nitrogen by 34.6%, while bulk density decreased by 8.4%. View evidence ↗

      What they found

      Applying biochar at 20 t ha⁻¹ led to significant improvements: organic carbon increased by 112%, water holding capacity by 22.7%, CEC by 18.6%, and available nitrogen by 34.6%, while bulk density decreased by 8.4%.

      In the paper's own words

      “Biochar at 20 t ha⁻¹ increased soil organic carbon by 112%, WHC by 22.7%, CEC by 18.6%, and available N by 34.6% while reducing bulk density by 8.4%.”

      Page 1

      Found in: Introduction

      Read it in the full textOpen PDF at page 1 ↗
    • All measured soil properties showed a dose-dependent improvement as the amount of biochar increased. View evidence ↗

      What they found

      All measured soil properties showed a dose-dependent improvement as the amount of biochar increased.

      In the paper's own words

      “All soil properties improved dose-dependently with biochar (Table 1).”

      Page 2

      Found in: Results

      Read it in the full textOpen PDF at page 2 ↗
    • The improvement in soil properties was mostly linear for application rates between 5 and 15 t ha⁻¹, but returns diminished at rates above 15 t ha⁻¹. View evidence ↗

      What they found

      The improvement in soil properties was mostly linear for application rates between 5 and 15 t ha⁻¹, but returns diminished at rates above 15 t ha⁻¹.

      In the paper's own words

      “Response was largely linear between 5-15 t ha⁻¹ with diminishing returns above 15.”

      Page 2

      Found in: Results

      Read it in the full textOpen PDF at page 2 ↗
  5. What it means

    • The authors conclude that biochar rates of 10-20 t ha⁻¹ improve all measured soil properties, with 15 t ha⁻¹ being the most cost-effective rate. View evidence ↗

      What it means

      The authors conclude that biochar rates of 10-20 t ha⁻¹ improve all measured soil properties, with 15 t ha⁻¹ being the most cost-effective rate.

      In the paper's own words

      “Biochar at 10-20 t ha⁻¹ improved all measured soil properties. The 15 t ha⁻¹ rate offers the best cost-benefit balance.”

      Page 3

      Found in: Conclusion

      Read it in the full textOpen PDF at page 3 ↗
    • Rice-husk biochar is recommended as a locally available and cost-effective solution for improving degraded sandy loam soils. View evidence ↗

      What it means

      Rice-husk biochar is recommended as a locally available and cost-effective solution for improving degraded sandy loam soils.

      In the paper's own words

      “Rice-husk biochar is a locally available, cost-effective amendment for degraded sandy loam soils with an estimated payback of 3.2 years.”

      Page 3

      Found in: Conclusion

      Read it in the full textOpen PDF at page 3 ↗

Visual summary

2 visuals

Illustrations explain the paper; charts are replotted from the paper's own table values.

AI-generated illustration
AI-generated conceptual illustration (sandy loam soil with biochar particles). It explains the idea and does not show study data.↗ Enlarge
Biochar Soil Mechanism
AI-generated conceptual illustration (sandy loam soil with biochar particles). It explains the idea and does not show study data.

AI-generated conceptual illustration (sandy loam soil with biochar particles). It explains the idea and does not show study data.

Open full-size image ↗

Biochar Soil Mechanism

AI-generated conceptual illustration (sandy loam soil with biochar particles). It explains the idea and does not show study data.

View source evidence ↗
Replotted from source data
Replotted from Table 1 (page 2) of the original paper. Every bar is the paper's own table value.↗ Enlarge
Bulk dens. (g cm⁻³): Control vs 5 t ha⁻¹ vs 10 t ha⁻¹ vs 15 t ha⁻¹ vs 20 t ha⁻¹
Replotted from Table 1 (page 2) of the original paper. Every bar is the paper's own table value.

Replotted from Table 1 (page 2) of the original paper. Every bar is the paper's own table value.

Open full-size image ↗

Bulk dens. (g cm⁻³): Control vs 5 t ha⁻¹ vs 10 t ha⁻¹ vs 15 t ha⁻¹ vs 20 t ha⁻¹

Replotted from Table 1 (page 2) of the original paper. Every bar is the paper's own table value.

View source evidence ↗

Figures & tables

From the original paper
Soil properties after two years of biochar application (pooled across sites)Table 1Page 2Soil organic carbon and available nitrogen across biochar ratesFigure 1Page 2Percentage change in soil properties at 20 t ha⁻¹ biochar versus controlFigure 2Page 2Research timeline for the biochar application experimentFigure 3Page 3
FULL TEXT Original article · reflowed for reading

Introduction

There's an old saying among soil scientists: "You can add nutrients to poor soil, but you can't easily add structure." Biochar challenges that by doing both [1]. Its porous structure improves water retention, while its cation exchange sites hold nutrients against leaching [2]. Sandy loam soils in the Indo-Gangetic Plains are particularly in need of these improvements because their low organic carbon results in poor water and nutrient retention [3]. This research quantified the dose-response relationship between rice-husk biochar and changes in soil properties at two representative sandy loam sites in Punjab and Uttar Pradesh [4, 5].

Baseline soil characterisation Pre-treatment soil at KVAU Ludhiana (30°54′N, 75°48′E) was a Typic Ustipsamment (sandy loam, 68% sand), pH 7.8, OC 0.41%, bulk density 1.52 g cm⁻³, CEC 8.4 cmol kg⁻¹. The NDUAT Kumarganj site (26°47′N, 82°12′E) had similar texture, pH 7.4, OC 0.44% [3, 4].

Material And Methods

Material Rice-husk biochar was produced by slow pyrolysis at 450°C for 2 hours. Properties: pH 9.2, carbon 48.3%, BET surface area 24.7 m² g⁻¹, CEC 28.4 cmol kg⁻¹. Biochar was crushed to <2 mm and incorporated into the top 15 cm before kharif rice 2021 [1, 2].

Methods

Five treatments (control, biochar at 5, 10, 15, 20 t ha⁻¹) in RCBD with four replications at each site. Two rice-wheat cycles (2021-2023). Soil sampled at 0-15 cm after each harvest. Bulk density, porosity, WHC, OC, CEC, available N and P by standard methods [5, 6].

Combined ANOVA in SAS 9.4, Tukey's HSD at p<0.05 [7]. Economic and sustainability assessment At 20 t ha⁻¹, application cost was ₹64,000 ha⁻¹. Combined benefits (15-20% fertiliser savings, improved WHC, 12-18% wheat yield increase) give estimated payback of 3.2 years and 10-year BCR of 2.4 [1, 4]. IJAN 2025; 7(2): 154-156 Hari Rana Department of Soil Science, Krishi Vigyan Agricultural University, Ludhiana, Punjab, India Zubin Dixit Department of Soil and Water Conservation, Narendra Deva University of Agriculture and Technology, Kumarganj, Uttar Pradesh, India Dheeraj Tyagi Department of Soil and Water Conservation, Narendra Deva University of Agriculture and Technology, Kumarganj, Uttar Pradesh, India Vandana Ojha Department of Soil and Water Conservation, Narendra Deva University of Agriculture and Technology, Kumarganj, Uttar Pradesh, India Hari Rana Department of Soil Science, Krishi Vigyan Agricultural University, Ludhiana, Punjab, India https://www.agriculturejournal.net

Results

Table 1: Soil properties after two years of biochar application (pooled across sites) Treatment Bulk dens. (g cm⁻³) Porosity (%) WHC (%) OC (%) CEC (cmol kg⁻¹) Avail N (kg ha⁻¹) Control 1.52 ± 0.03a 42.6 ± 1.1c 28.4 ± 1.2d 0.41 ± 0.03d 8.4 ± 0.4d 162 ± 8c 5 t ha⁻¹ 1.47 ± 0.03ab 44.8 ± 1.2bc 30.8 ± 1.1cd 0.54 ± 0.04c 9.1 ± 0.5cd 178 ± 9bc 10 t ha⁻¹ 1.43 ± 0.02b 46.2 ± 1.0b 32.4 ± 1.3bc 0.68 ± 0.04b 9.8 ± 0.4bc 194 ± 10b 15 t ha⁻¹ 1.41 ± 0.02bc 47.1 ± 0.9ab 34.1 ± 1.2ab 0.79 ± 0.05ab 10.4 ± 0.5ab 208 ± 11ab 20 t ha⁻¹ 1.39 ± 0.02c 48.6 ± 0.8a 34.8 ± 1.1a 0.87 ± 0.05a 10.0 ± 0.5a 218 ± 12a Different letters within columns differ at p<0.05. Values are means ± SE (n = 8) All soil properties improved dose-dependently with biochar (Table 1). At 20 t ha⁻¹, OC more than doubled and available N rose by 34.6%. Response was largely linear between 5-15 t ha⁻¹ with diminishing returns above 15.

Table 1. Soil properties after two years of biochar application (pooled across sites)
TreatmentBulk dens. (g cm⁻³)Porosity (%)WHC (%)OC (%)CEC (cmol kg⁻¹)Avail N (kg ha⁻¹)
Control1.52 ± 0.03a42.6 ± 1.1c28.4 ± 1.2d0.41 ± 0.03d8.4 ± 0.4d162 ± 8c
5 t ha⁻¹1.47 ± 0.03ab44.8 ± 1.2bc30.8 ± 1.1cd0.54 ± 0.04c9.1 ± 0.5cd178 ± 9bc
10 t ha⁻¹1.43 ± 0.02b46.2 ± 1.0b32.4 ± 1.3bc0.68 ± 0.04b9.8 ± 0.4bc194 ± 10b
15 t ha⁻¹1.41 ± 0.02bc47.1 ± 0.9ab34.1 ± 1.2ab0.79 ± 0.05ab10.4 ± 0.5ab208 ± 11ab
20 t ha⁻¹1.39 ± 0.02c48.6 ± 0.8a34.8 ± 1.1a0.87 ± 0.05a10.0 ± 0.5a218 ± 12a

Table text extracted from the original PDF; superscript letters are shown inline. The original table image is below.

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Soil properties after two years of biochar application (pooled across sites)↗ Enlarge
Table 1
Soil properties after two years of biochar application (pooled across sites)

Soil properties after two years of biochar application (pooled across sites)

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Original paper tableSource PDF · page 2 ↗

Fig 1: Soil organic carbon and available nitrogen across biochar rates Fig 2: Percentage change in soil properties at 20 t ha⁻¹ biochar versus control https://www.agriculturejournal.net 5. Jeffery S, Verheijen FGA, van der Velde M, Bastos AC. Effects of biochar on crop productivity: meta- analysis. Agriculture Ecosystems and Environment. 2011;144(1):175-187. 6.

Figure 2. Percentage change in soil properties at 20 t ha⁻¹ biochar versus control
Percentage change in soil properties at 20 t ha⁻¹ biochar versus control↗ Enlarge
Figure 2
Percentage change in soil properties at 20 t ha⁻¹ biochar versus control

Percentage change in soil properties at 20 t ha⁻¹ biochar versus control

Open full-size image ↗
Original paper figureSource PDF · page 2 ↗
Figure 1. Soil organic carbon and available nitrogen across biochar rates
Soil organic carbon and available nitrogen across biochar rates↗ Enlarge
Figure 1
Soil organic carbon and available nitrogen across biochar rates

Soil organic carbon and available nitrogen across biochar rates

Open full-size image ↗
Original paper figureSource PDF · page 2 ↗

Jackson ML. Soil Chemical Analysis. Prentice Hall, Englewood Cliffs. 1973. 7. Gomez KA, Gomez AA.

Statistical Procedures for Agricultural Research. Wiley, New York. 1984. 8. Woolf D, Amonette JE, Street-Perrott FA, Lehmann J, Joseph S. Sustainable biochar to mitigate climate change.

Nature Communications. 2010;1:56. 9. Sohi SP, Krull E, Lopez-Capel E, Bol R. Biochar use and function in soil: a review. Advances in Agronomy. 2010;105:47-82. 10.

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Impact of biochar on quality of a Midwestern soil. Geoderma. 2010;158(3-4):443-449. 12. Novak JM, Busscher WJ, Laird DL, Ahmedna M, Watts DW, Niandou MAS. Impact of biochar on fertility of a southeastern coastal plain soil.

Soil Science. 2009;174(2):105-112. 13. Chan KY, Van Zwieten L, Meszaros I, Downie A, Joseph S. Agronomic values of greenwaste biochar. Australian Journal of Soil Research. 2007;45(8):629- 634. 14.

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Biochar effects on plant productivity: A meta-analysis. GCB Bioenergy. 2013;5(2):202-214. Fig 3: Research timeline for the biochar application experiment

Figure 3. Research timeline for the biochar application experiment
Research timeline for the biochar application experiment↗ Enlarge
Figure 3
Research timeline for the biochar application experiment

Research timeline for the biochar application experiment

Open full-size image ↗
Original paper figureSource PDF · page 3 ↗

Discussion

The 112% OC increase at 20 t ha⁻¹ reflects biochar's high carbon stability (>100 years residence time) [1, 2]. The 22.7% WHC improvement could bridge 2-3 extra days between irrigations in sandy loam [3]. The CEC increase (18.6%) reflects oxidised surface functional groups [4]. Effects were consistent across both sites, suggesting broad applicability across Indo-Gangetic sandy loams.

Conclusion

Biochar at 10-20 t ha⁻¹ improved all measured soil properties. The 15 t ha⁻¹ rate offers the best cost-benefit balance. Rice-husk biochar is a locally available, cost- effective amendment for degraded sandy loam soils with an estimated payback of 3.2 years.

Acknowledgements

Funding sources Supported by KVAU Ludhiana and NDUAT Kumarganj internal funds. Institutional support The authors thank both universities for field and laboratory facilities. Contributions not qualifying for authorship Thanks to Mr. Gurpreet Singh for biochar production.

References

4 in the original paper
  1. Lehmann J, Joseph S. Biochar for Environmental Management. Second edition. Routledge, London. 2015.
  2. Glaser B, Lehmann J, Zech W. Ameliorating physical and chemical properties of highly weathered soils with charcoal. Biology and Fertility of Soils. 2002;35(4):219-230.
  3. Aggarwal P, Sharma NK. Water retention characteristics of some Indian soils. Indian Journal of Agricultural Sciences. 2002;72(2):73-78.
  4. Major J, Rondon M, Molina D, Riha SJ, Lehmann J. Maize yield and nutrition after biochar application. Plant and Soil. 2010;333(1):117-128.