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Research article · 2025 · Full text

International Journal of Geography Geology and Environment

Analysis of soil compaction effects on root growth and infiltration in the Punjab croplands

Meena BoseDilip Mahajan

Volume 7(6) · Pages 144–146 · DOI: 10.22271/27067483.2025.v7.i6c.725 ↗

Research areasSoil Management and Crop YieldSoil and Unsaturated FlowSoil erosion and sediment transport

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Abstract

Author-written

Heavy tractors and repeated tillage passes have quietly compressed the soils beneath India's breadbasket. This research measured the effects of soil compaction on wheat root growth and water infiltration across five tillage treatments at 12 experimental plots in the Punjab croplands of Northwestern India. Bulk density, penetration resistance, root length density, and steady-state infiltration rate were measured over two cropping seasons (rabi 2021–2022 and 2022–2023). Bulk density ranged from 1.31 g/cm³ under deep ripping to 1.64 g/cm³ in subsoil-compacted plots. Root length density showed a strong negative correlation with bulk density (r = –0.81, p < 0.001), declining from 14.7 cm/cm³ in the least compacted treatment to 6.3 cm/cm³ in the most compacted. Infiltration rates fell from 28.4 mm/hr to 8.7 mm/hr across the same gradient. No-till plots maintained intermediate values (bulk density 1.38 g/cm³, infiltration 21.6 mm/hr), suggesting that eliminating tillage traffic can partly mitigate compaction without deep ripping. These data support policy recommendations for controlled traffic farming in the Punjab to maintain both root access and water entry into the soil profile.

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

    • Soil compaction is a gradual process caused by machinery traffic that can lead to severe waterlogging and root restriction, often remaining unnoticed until yields are affected. View evidence ↗

      Why it matters

      Soil compaction is a gradual process caused by machinery traffic that can lead to severe waterlogging and root restriction, often remaining unnoticed until yields are affected.

      In the paper's own words

      “Soil compaction is agriculture's hidden yield thief. Unlike drought or pest damage, compaction operates underground and builds gradually over years of machinery traffic, making it easy to overlook until root restriction and waterlogging become severe”

      Page 1

      Found in: Introduction

      Read it in the full textOpen PDF at page 1 ↗
    • In the Punjab region, five decades of wheat-rice rotation and repeated tractor passes have compacted soils to depths between 30 and 45 cm. View evidence ↗

      Why it matters

      In the Punjab region, five decades of wheat-rice rotation and repeated tractor passes have compacted soils to depths between 30 and 45 cm.

      In the paper's own words

      “In the Indo-Gangetic Plains of Punjab, where wheat-rice rotation has dominated for over five decades, tractor passes during field preparation, sowing, spraying, and harvest compact soils to depths of 30–45 cm”

      Page 1

      Found in: Introduction

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

    • The study aimed to quantify the relationship between soil compaction, root growth, and water infiltration to find the best management strategy for Punjab's croplands. View evidence ↗

      The question

      The study aimed to quantify the relationship between soil compaction, root growth, and water infiltration to find the best management strategy for Punjab's croplands.

      In the paper's own words

      “This research compared root growth and infiltration responses across five tillage treatments over two seasons, aiming to quantify the compaction-root-infiltration chain and identify the most effective management option for Punjab conditions”

      Page 1

      Found in: Introduction

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

    • The research employed a randomised complete block design with 12 total plots across three districts: Ludhiana, Jalandhar, and Amritsar. View evidence ↗

      What they did

      The research employed a randomised complete block design with 12 total plots across three districts: Ludhiana, Jalandhar, and Amritsar.

      In the paper's own words

      “The experiment used a randomised complete block design with four replications at each of three sites in Ludhiana, Jalandhar, and Amritsar districts (12 plots total).”

      Page 1

      Found in: Field Experimental Design

      Read it in the full textOpen PDF at page 1 ↗
    • Five tillage treatments were tested: conventional tillage, no-till direct seeding, deep ripping to 45 cm, induced subsoil compaction via extra tractor passes, and a farmer practice control. View evidence ↗

      What they did

      Five tillage treatments were tested: conventional tillage, no-till direct seeding, deep ripping to 45 cm, induced subsoil compaction via extra tractor passes, and a farmer practice control.

      In the paper's own words

      “Five treatments were: (T1) conventional tillage (3 passes with 45 HP tractor), (T2) no-till direct seeding, (T3) deep ripping to 45 cm before sowing, (T4) induced subsoil compaction (6 additional tractor passes simulating heavy traffic), and (T5) farmer practice control.”

      Page 1

      Found in: Field Experimental Design

      Read it in the full textOpen PDF at page 1 ↗
    • The study used wheat variety HD-3086 over two rabi seasons (2021–2022 and 2022–2023), with sowing in November and harvesting in April. View evidence ↗

      What they did

      The study used wheat variety HD-3086 over two rabi seasons (2021–2022 and 2022–2023), with sowing in November and harvesting in April.

      In the paper's own words

      “Wheat (variety HD-3086) was sown in November and harvested in April for both seasons”

      Page 1

      “measured over two cropping seasons (rabi 2021–2022 and 2022–2023)”

      Page 1

      Found in: Field Experimental Design

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

    • Bulk density varied significantly by treatment, with the lowest value of 1.31 g/cm³ in deep ripping and the highest of 1.64 g/cm³ in subsoil-compacted plots. View evidence ↗

      What they found

      Bulk density varied significantly by treatment, with the lowest value of 1.31 g/cm³ in deep ripping and the highest of 1.64 g/cm³ in subsoil-compacted plots.

      In the paper's own words

      “Bulk density ranged from 1.31 g/cm³ under deep ripping to 1.64 g/cm³ in subsoil-compacted plots.”

      Page 1

      Found in: Discussion

      Read it in the full textOpen PDF at page 1 ↗
    • Root length density was strongly negatively correlated with bulk density (r = –0.81), dropping from 14.7 cm/cm³ in the least compacted soil to 6.3 cm/cm³ in the most compacted. View evidence ↗

      What they found

      Root length density was strongly negatively correlated with bulk density (r = –0.81), dropping from 14.7 cm/cm³ in the least compacted soil to 6.3 cm/cm³ in the most compacted.

      In the paper's own words

      “Root length density showed a strong negative correlation with bulk density (r = –0.81, p < 0.001), declining from 14.7 cm/cm³ in the least compacted treatment to 6.3 cm/cm³ in the most compacted.”

      Page 1

      Found in: Materials

      Read it in the full textOpen PDF at page 1 ↗
    • Water infiltration rates decreased from 28.4 mm/hr in the least compacted treatment to 8.7 mm/hr in the most compacted treatment. View evidence ↗

      What they found

      Water infiltration rates decreased from 28.4 mm/hr in the least compacted treatment to 8.7 mm/hr in the most compacted treatment.

      In the paper's own words

      “Infiltration rates fell from 28.4 mm/hr to 8.7 mm/hr across the same gradient.”

      Page 1

      Found in: Introduction

      Read it in the full textOpen PDF at page 1 ↗
    • No-till plots showed intermediate results, with a bulk density of 1.38 g/cm³ and infiltration of 21.6 mm/hr, indicating that removing tillage traffic can partially mitigate compaction. View evidence ↗

      What they found

      No-till plots showed intermediate results, with a bulk density of 1.38 g/cm³ and infiltration of 21.6 mm/hr, indicating that removing tillage traffic can partially mitigate compaction.

      In the paper's own words

      “No-till plots maintained intermediate values (bulk density 1.38 g/cm³, infiltration 21.6 mm/hr), suggesting that eliminating tillage traffic can partly mitigate compaction without deep ripping.”

      Page 1

      Found in: Discussion

      Read it in the full textOpen PDF at page 1 ↗
    • Subsoil compaction led to a 13.5% yield penalty compared to the control group due to restricted rooting volume. View evidence ↗

      What they found

      Subsoil compaction led to a 13.5% yield penalty compared to the control group due to restricted rooting volume.

      In the paper's own words

      “The yield penalty in the subsoil-compacted treatment (–13.5% vs control) reflects this restricted rooting volume.”

      Page 3

      Found in: Discussion

      Read it in the full textOpen PDF at page 3 ↗
    • Compared to deep ripping, no-till achieved 84% of the benefit for root growth and 76% for infiltration at a much lower cost. View evidence ↗

      What they found

      Compared to deep ripping, no-till achieved 84% of the benefit for root growth and 76% for infiltration at a much lower cost.

      In the paper's own words

      “No-till achieved 76% of the deep-ripping benefit in infiltration and 84% in root growth at negligible additional cost”

      Page 3

      Found in: Comprehensive Interpretation

      Read it in the full textOpen PDF at page 3 ↗
  5. What it means

    • The authors conclude that no-till management is the most practical strategy for mitigating soil compaction in the region due to its cost-effectiveness and intermediate physical benefits. View evidence ↗

      What it means

      The authors conclude that no-till management is the most practical strategy for mitigating soil compaction in the region due to its cost-effectiveness and intermediate physical benefits.

      In the paper's own words

      “No-till management achieves intermediate physical properties at lower cost, making it the most practical compaction mitigation strategy for the region.”

      Page 3

      Found in: Conclusion

      Read it in the full textOpen PDF at page 3 ↗
    • The authors recommend field-scale testing of controlled traffic farming, which uses permanent tramlines to confine machinery, to potentially further improve soil conditions. View evidence ↗

      What it means

      The authors recommend field-scale testing of controlled traffic farming, which uses permanent tramlines to confine machinery, to potentially further improve soil conditions.

      In the paper's own words

      “Controlled traffic farming — confining all machinery to permanent tramlines — could deliver further benefits and deserves field-scale testing in the wheat-rice rotation system.”

      Page 3

      Found in: Conclusion

      Read it in the full textOpen PDF at page 3 ↗

Visual summary

3 visuals

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

AI-generated illustration
AI-generated conceptual illustration (Wheat plants in Punjab cropland soil). It explains the idea and does not show study data.↗ Enlarge
Compaction Impact Chain
AI-generated conceptual illustration (Wheat plants in Punjab cropland soil). It explains the idea and does not show study data.

AI-generated conceptual illustration (Wheat plants in Punjab cropland soil). It explains the idea and does not show study data.

Open full-size image ↗

Compaction Impact Chain

AI-generated conceptual illustration (Wheat plants in Punjab cropland soil). 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
BD 0–15 (g/cm³): Conv. tillage vs No-till vs Deep ripping vs Subsoil compacted vs Control
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 ↗

BD 0–15 (g/cm³): Conv. tillage vs No-till vs Deep ripping vs Subsoil compacted vs Control

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

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
PR Max (MPa): Conv. tillage vs No-till vs Deep ripping vs Subsoil compacted vs Control
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 ↗

PR Max (MPa): Conv. tillage vs No-till vs Deep ripping vs Subsoil compacted vs Control

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 physical properties and root parameters by treatment (mean of 2 seasons, 3 sites)Table 1Page 2Pearson correlation matrix (n = 120)Table 2Page 2Violin plots of bulk density distribution across the five tillage treatments.Figure 1Page 2Scatter plot of bulk density vs root length density with linearFigure 2Page 3
FULL TEXT Original article · reflowed for reading

Introduction

Soil compaction is agriculture's hidden yield thief. Unlike drought or pest damage, compaction operates underground and builds gradually over years of machinery traffic, making it easy to overlook until root restriction and waterlogging become severe [1] . In the Indo-Gangetic Plains of Punjab, where wheat-rice rotation has dominated for over five decades, tractor passes during field preparation, sowing, spraying, and harvest compact soils to depths of 30-45 cm [2] . And the machinery is getting heavier: average tractor weight in Punjab increased from 1, 800 kg in 1990 to 2, 600 kg by 2020, amplifying the compaction load per axle [3] . Root systems are the first casualties. When bulk density exceeds roughly 1.55 g/cm³ in loamy soils, root elongation slows markedly because mechanical impedance exceeds the roots' ability to push through soil pores [4] . Simultaneously, compaction reduces macroporosity and infiltration capacity, promoting surface ponding and anaerobic conditions that further inhibit root function [5] . Earlier research in the Punjab documented yield penalties of 8-15% attributable to compaction in rice fields, but comparable data for the rabi wheat crop were sparse [6] . This research compared root growth and infiltration responses across five tillage treatments over two seasons, aiming to quantify the compaction-root-infiltration chain and identify the most effective management option for Punjab conditions [7] .

Field Experimental Design

The experiment used a randomised complete block design with four replications at each of three sites in Ludhiana, Jalandhar, and Amritsar districts (12 plots total). Five treatments were: (T 1 ) conventional tillage (3 passes with 45 HP tractor), (T 2 ) no-till direct seeding, (T 3 ) deep ripping to 45 cm before sowing, (T 4 ) induced subsoil compaction (6 additional tractor passes simulating heavy traffic), and (T 5 ) farmer practice control. Plot size was 10 × 8 m. Wheat (variety HD-3086) was sown in November and harvested in April for both seasons [8] .

Materials and Methods

Materials and Methods

Materials

Field measurements were taken during rabi 2021-2022 and 2022-2023 at the three Punjab sites, coordinated from the Hyderabad Centre for Geological Research, Telangana, India. Soil samples for bulk density were collected using 100 cm³ steel cores at 0-15 and 15-30 cm depth at three positions per plot (36 cores per treatment per season). Penetration resistance was measured with a hand-held cone penetrometer (Eijkelkamp, 30° cone, 1 cm² base area) at 5 cm depth intervals to 50 cm. Root samples were taken at heading stage by driving 7.5 cm diameter soil cores to 40 cm and washing roots over a 0.5 mm sieve [9] .

Methods

Root length density (cm root per cm³ soil) was estimated using the line-intersect method. Steady-state infiltration rate was measured with double-ring infiltrometers (30/60 cm diameter) at three positions per plot, allowing 60 minutes of pre-wetting before recording the steady rate over 30 minutes. Data were analysed by two-way ANOVA (treatment × season) with Tukey's HSD post-hoc test at α = 0.05 in R v4.2. Pearson correlations were computed between bulk density, root length density, infiltration rate, and penetration resistance [10,11] .

Baseline Soil Characterisation

Pre-experiment soil analysis (October 2021) showed loam to clay-loam texture across the three sites, with sand 34-42%, silt 28-36%, and clay 24-32%. Organic carbon ranged from 0.48% to 0.67%, pH from 7.6 to 8.1, and EC from 0.31 to 0.52 dS/m. Pre-treatment bulk density averaged 1.42±0.06 g/cm³ at 0-15 cm and 1.48±0.07 g/cm³ at 15-30 cm. .94 All treatment differences were significant (p < 0.05) except between no-till and control for BD at 0-15 cm (p = 0.08).

Results

Results

Comprehensive Interpretation

The correlation matrix confirms tight coupling between compaction (BD, PR), root growth (RLD), and water entry (infiltration). Deep ripping produced the best physical conditions but is expensive (about ₹3, 200/ha per season).

No-till achieved 76% of the deep-ripping benefit in infiltration and 84% in root growth at negligible additional cost, making it the most cost-effective option for widespread adoption.

Discussion

The bulk density threshold at which wheat root elongation declines sharply appears to lie near 1.55 g/cm³ in these loamy soils, consistent with the 1.55-1.60 range reported by Lipiec and Hatano [4] for temperate loams. Above this threshold, penetration resistance exceeds 2.5 MPa and roots are physically unable to explore the subsoil, restricting water and nutrient uptake to the shallow zone [12] . The yield penalty in the subsoil-compacted treatment (-13.5% vs control) reflects this restricted rooting volume.

No-till's intermediate performance is encouraging because it eliminates the primary source of compactionrepeated tractor passes during seedbed preparationwhile relying on biological processes (root channels, earthworm burrows) to gradually improve subsoil structure [13] . The 21.6 mm/hr infiltration rate in no-till plots, though lower than deep ripping, comfortably exceeds the 90th-percentile rainfall intensity of 18 mm/hr recorded at the nearest meteorological station, meaning that surface ponding should be rare.

Conclusion

Soil compaction in Punjab wheat fields raises bulk density to 1.64 g/cm³, reduces root length density by 57%, and cuts infiltration by 69% compared to deep-ripped soils. No-till management achieves intermediate physical properties at lower cost, making it the most practical compaction mitigation strategy for the region. Controlled traffic farming confining all machinery to permanent tramlinescould deliver further benefits and deserves field-scale testing in the wheat-rice rotation system.

Acknowledgement

Acknowledgements Funding SourcesSupported by research funds at the Hyderabad Centre for Geological Research. Institutional SupportThe Department of Environmental Studies provided field equipment and laboratory access.

Figures and tables from the paper

Table 1. Soil physical properties and root parameters by treatment (mean of 2 seasons, 3 sites)
TreatmentBD 0–15 (g/cm³)BD 15–30PR Max (MPa)RLD (cm/cm³)Infil. (mm/hr)Yield (t/ha)
Conv. tillage1.52±0.041.58±0.052.349.8±1.714.2±3.14.87
No-till1.38±0.051.44±0.061.8712.4±2.121.6±4.25.12
Deep ripping1.31±0.041.36±0.051.5214.7±2.428.4±5.15.38
Subsoil compacted1.64±0.061.71±0.073.186.3±1.38.7±2.44.21
Control1.45±0.051.51±0.062.1210.6±1.916.8±3.64.94

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

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Soil physical properties and root parameters by treatment (mean of 2 seasons, 3 sites)↗ Enlarge
Table 1
Soil physical properties and root parameters by treatment (mean of 2 seasons, 3 sites)

Soil physical properties and root parameters by treatment (mean of 2 seasons, 3 sites)

Open full-size image ↗
Original paper tableSource PDF · page 2 ↗
Table 2. Pearson correlation matrix (n = 120)
VariableBDPRRLDInfiltration
BD1.000.87**–0.81**–0.78**
PR0.87**1.00–0.76**–0.72**
RLD–0.81**–0.76**1.000.69**
Infiltration–0.78**–0.72**0.69**1.00

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

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Pearson correlation matrix (n = 120)↗ Enlarge
Table 2
Pearson correlation matrix (n = 120)

Pearson correlation matrix (n = 120)

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Original paper tableSource PDF · page 2 ↗
Figure 1. Violin plots of bulk density distribution across the five tillage treatments.
Violin plots of bulk density distribution across the five tillage treatments.↗ Enlarge
Figure 1
Violin plots of bulk density distribution across the five tillage treatments.

Violin plots of bulk density distribution across the five tillage treatments.

Open full-size image ↗
Original paper figureSource PDF · page 2 ↗
Figure 2. Scatter plot of bulk density vs root length density with linear
Scatter plot of bulk density vs root length density with linear↗ Enlarge
Figure 2
Scatter plot of bulk density vs root length density with linear

Scatter plot of bulk density vs root length density with linear

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

References

18 in the original paper
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