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Research article · 2024 · Full text

International Journal of Research in Agronomy

Characteristics of west coast lateritic soils of Southern India

Mallikarjuna LingappaBT Naveen KumarT. J. RameshaR RashmiKedarnath Kedarnath

Volume 7(3) · Pages 659–664 · DOI: 10.33545/2618060x.2024.v7.i3i.496 ↗

Research areasGeotechnical and construction materials studies

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Abstract

Author-written

Background: Soil fertility is meant for understanding the nutrient requirements, based on fertility status of soils to achieve good crop yields. Soil fertility, compact-ability and erodibility are the domains of soil quality. Among these, the problem of decline in soil fertility compromises maximum productivity. Depletion in soil fertility is the hugest serious due to cropping pattern, leaching, erosion etc., causes loss of considerable amount of nutrients annually. In order to notice information on current soil fertility status, this study was accompanied in different Talukas of Dakhsina Kannada district of coastal Karnataka. Methods: Characterized the soils for fertility status by taking fifty representative samples from each taluk of Dakshina Kannada district in coastal Karnataka to recommend chemical and organic fertilizers applications based on the present soil nutrient status for the farming community.Results: The soils were persisted acidic in reaction, with very low salt content, medium to high in organic carbon status. The available macronutrients of the soil samples indicated that the nitrogen and potassium low to medium in all the Talukas, and low in available phosphorous and Sulphur. Among the DTPA extractable micronutrients, iron and manganese were in high in most samples collected, available copper was adequate and available zinc was also sufficient except in soil samples of Bantwal Taluk. The available boron was found to be low in soils of all the talukas of the district.

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

    • Declining soil fertility is a critical issue because it limits the maximum productivity of crops. View evidence ↗

      Why it matters

      Declining soil fertility is a critical issue because it limits the maximum productivity of crops.

      In the paper's own words

      “Among these, the problem of decline in soil fertility compromises maximum productivity.”

      Page 1

      Found in: Introduction

      Read it in the full textOpen PDF at page 1 ↗
    • Soil fertility is depleted annually through processes such as erosion, leaching, and specific cropping patterns. View evidence ↗

      Why it matters

      Soil fertility is depleted annually through processes such as erosion, leaching, and specific cropping patterns.

      In the paper's own words

      “Depletion in soil fertility is the hugest serious due to cropping pattern, leaching, erosion etc., causes loss of considerable amount of nutrients annually.”

      Page 1

      Found in: Introduction

      Read it in the full textOpen PDF at page 1 ↗
    • The Dakshina Kannada district in coastal Karnataka has an economy primarily based on industry and horticulture. View evidence ↗

      Why it matters

      The Dakshina Kannada district in coastal Karnataka has an economy primarily based on industry and horticulture.

      In the paper's own words

      “Dakshina Kannada is one of the three coastal districts of the state with predominantly horticultural and industrial economy.”

      Page 1

      Found in: Introduction

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

    • The study aimed to determine the current soil fertility status across different Talukas of the Dakshina Kannada district. View evidence ↗

      The question

      The study aimed to determine the current soil fertility status across different Talukas of the Dakshina Kannada district.

      In the paper's own words

      “In order to notice information on current soil fertility status, this study was accompanied in different Talukas of Dakhsina Kannada district of coastal Karnataka.”

      Page 1

      Found in: Introduction

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

    • The study measured pH, electrical conductivity, organic carbon, nitrogen, phosphorus, potassium, and sulphur using established standard chemical extraction and estimation methods. View evidence ↗

      What they did

      The study measured pH, electrical conductivity, organic carbon, nitrogen, phosphorus, potassium, and sulphur using established standard chemical extraction and estimation methods.

      In the paper's own words

      “Electrical conductivity, pH, organic carbon, were determined by standard methods (Jackson 1973) [3]. Available nitrogen was estimated by alkaline permanganate method (Subbaiah and Asija, 1956) [13]. For available phosphorus determination, extraction was done using Brays extractant and then subsequent estimation by Jackson, (1973) [3] method. Available potassium was extracted using neutral normal ammonium acetate and measured with flame photometer (Jackson, 1973) [3]. Sulphur was extracted using 0.15 percent CaCl2 solution”

      Page 2

      Found in: Materials and Methods

      Read it in the full textOpen PDF at page 2 ↗
    • Micronutrients (Fe, Cu, Mn, Zn) were measured via DTPA extraction and atomic absorption spectrophotometry, while Boron was measured via hot water extraction. View evidence ↗

      What they did

      Micronutrients (Fe, Cu, Mn, Zn) were measured via DTPA extraction and atomic absorption spectrophotometry, while Boron was measured via hot water extraction.

      In the paper's own words

      “Available micronutrients such as iron, copper, manganese and zinc were extracted using standard DTPA extract at pH 7.3 and the concentration was measured in an atomic absorption spectrophotometer (Lindsay and Norvell, 1978) [4]. Boron (Hot water extraction), particle size analysis by international pipette method”

      Page 2

      Found in: Materials and Methods

      Read it in the full textOpen PDF at page 2 ↗
  4. What they found

    • Soils across all six Talukas were moderate to strongly acidic, with pH values ranging from a low of 4.9 in Sullia to a high of 5.7 in Puttur. View evidence ↗

      What they found

      Soils across all six Talukas were moderate to strongly acidic, with pH values ranging from a low of 4.9 in Sullia to a high of 5.7 in Puttur.

      In the paper's own words

      “Soils of all the six Taluks were moderate to strongly acidic with highest average soil pH of 5.7 was recorded in Puttur Taluk (Fig. v) and lowest average pH of 4.9 was in soils of Sullia Taluk (Fig. ix).”

      Page 2

      Found in: Physico-chemical properties

      Read it in the full textOpen PDF at page 2 ↗
    • Organic carbon content was high in all Talukas, with average values between 7.6 g kg-1 and 11.2 g kg-1. View evidence ↗

      What they found

      Organic carbon content was high in all Talukas, with average values between 7.6 g kg-1 and 11.2 g kg-1.

      In the paper's own words

      “The average organic carbon content of the soils varied from 7.6 g kg-1 soil to 11.2 g kg-1 soil and was found to be high in all Taluks of the district.”

      Page 2

      Found in: Physico-chemical properties

      Read it in the full textOpen PDF at page 2 ↗
    • Available nitrogen was rated low to medium, ranging from 212.4 kg ha-1 in Moodabidri to 388.4 kg ha-1 in Puttur. View evidence ↗

      What they found

      Available nitrogen was rated low to medium, ranging from 212.4 kg ha-1 in Moodabidri to 388.4 kg ha-1 in Puttur.

      In the paper's own words

      “The available nitrogen content in all the Taluks was rated as low to medium with highest average of 388.4 kg ha-1 was recorded in soils of Puttur Taluk (Fig. vi) and lowest average of 212.4 kg ha-1 was recorded in soils of Moodabidri Taluk (Fig. xii).”

      Page 3

      Found in: Available macronutrients

      Read it in the full textOpen PDF at page 3 ↗
    • Available phosphorus was rated as low across all Talukas, with averages between 16.2 and 21.8 kg ha-1. View evidence ↗

      What they found

      Available phosphorus was rated as low across all Talukas, with averages between 16.2 and 21.8 kg ha-1.

      In the paper's own words

      “The available phosphorus content in soils of all Taluks averages varied from 16.2 to 21.8 kg ha-1 and was rated as low.”

      Page 3

      Found in: Available macronutrients

      Read it in the full textOpen PDF at page 3 ↗
    • Available sulphur was rated as very low in most soils, with averages between 7.74 and 9.51 mg kg-1. View evidence ↗

      What they found

      Available sulphur was rated as very low in most soils, with averages between 7.74 and 9.51 mg kg-1.

      In the paper's own words

      “The average available sulphur in the soils varied from 7.74 to 9.51 mg kg-1 and most of the soils were very low in ratings.”

      Page 3

      Found in: Available macronutrients

      Read it in the full textOpen PDF at page 3 ↗
    • Zinc levels (0.58 to 1.03 mg kg-1) were sufficient in most areas, except for the soils in Bantwal Taluk. View evidence ↗

      What they found

      Zinc levels (0.58 to 1.03 mg kg-1) were sufficient in most areas, except for the soils in Bantwal Taluk.

      In the paper's own words

      “DTPA extractable Zn average ranged from 0.58 to 1.03 mg kg-1 soil... these soils could be classified as Sufficient in Zn except soils of Bantwal Taluk.”

      Page 4

      Found in: Available micronutrients

      Read it in the full textOpen PDF at page 4 ↗
    • The soils were rich in available iron, with DTPA extractable Fe ranging from 39.7 to 52.4 mg kg-1. View evidence ↗

      What they found

      The soils were rich in available iron, with DTPA extractable Fe ranging from 39.7 to 52.4 mg kg-1.

      In the paper's own words

      “The DTPA extractable Fe content varied from 39.7 to 52.4 mg kg-1 soil... the soils were rich in available iron.”

      Page 4

      Found in: Available micronutrients

      Read it in the full textOpen PDF at page 4 ↗
    • Available manganese was high in all Talukas, with mean values between 3.15 and 4.45 mg kg-1. View evidence ↗

      What they found

      Available manganese was high in all Talukas, with mean values between 3.15 and 4.45 mg kg-1.

      In the paper's own words

      “Mean available Mn varied from 3.15 to 4.45 mg kg-1 soil and was found to be high in soils of all the Talukas.”

      Page 4

      Found in: Available micronutrients

      Read it in the full textOpen PDF at page 4 ↗
    • Available boron was low (0.24 mg kg-1), which the authors link to nut cracking and nut fall in areca nut fields. View evidence ↗

      What they found

      Available boron was low (0.24 mg kg-1), which the authors link to nut cracking and nut fall in areca nut fields.

      In the paper's own words

      “Most of the soils of Dakshina Kannada were found low in available Boron (0.24 mg kg-1) hence there was extreme nut fall and nut cracking in some of the areca nut growing fields.”

      Page 4

      Found in: Available micronutrients

      Read it in the full textOpen PDF at page 4 ↗
  5. What it means

    • The authors conclude that deficient nutrients must be restored using organic manures or chemical fertilizers to ensure sustainable crop production. View evidence ↗

      What it means

      The authors conclude that deficient nutrients must be restored using organic manures or chemical fertilizers to ensure sustainable crop production.

      In the paper's own words

      “The deficient nutrients have to be restored through chemical fertilizers and/or organic manures to maintain soil health for efficient and sustainable crop production in these soils.”

      Page 5

      Found in: Conclusions

      Read it in the full textOpen PDF at page 5 ↗

Visual summary

1 visuals

Illustrations explain the paper; they do not show study data.

AI-generated illustration
AI-generated conceptual illustration (lateritic soils of the coastal region of Southern India). It explains the idea and does not show study data.↗ Enlarge
Study Area and Sampling
AI-generated conceptual illustration (lateritic soils of the coastal region of Southern India). It explains the idea and does not show study data.

AI-generated conceptual illustration (lateritic soils of the coastal region of Southern India). It explains the idea and does not show study data.

Open full-size image ↗

Study Area and Sampling

AI-generated conceptual illustration (lateritic soils of the coastal region of Southern India). It explains the idea and does not show study data.

View source evidence ↗

Figures & tables

From the original paper
Ranges and means of physical, chemical and physicochemicalTable 1Page 2pH, EC and Organic matter status of Bantwal TalukFigure 1Page 2Primary nutrient status of Bantwal TalukFigure 2Page 2pH, EC and Organic Carbon status in soils of Belthangady TalukFigure 3Page 3Primary nutrient status in soils of Belthangady TalukFigure 4Page 3pH, EC and Organic carbon status in soils of Puttur TalukFigure 5Page 3Primary nutrient status in soils of Puttur TalukFigure 6Page 3pH, EC and Organic carbon status in soils of Sullia TalukFigure 7Page 3Primary nutrient status in soils of Sullia TalukFigure 8Page 4pH, EC and Organic carbon status in soils of Moodabidri TalukFigure 9Page 4Primary nutrient status in soils of Moodabidre TalukFigure 10Page 4Secondary and Micronutrient status in soils of Bantwal TalukFigure 11Page 4Secondary and Micronutrient status in soils of BelthangadyFigure 12Page 4Secondary and Micronutrient status in soils of Puttur TalukFigure 13Page 5Secondary and Micronutrient status in soils of Puttur TalukFigure 14Page 5Secondary and Micronutrient status in soils of Kadaba TalukFigure 15Page 5Secondary and Micronutrient status in soils of Sullia TalukFigure 16Page 5Secondary and Micronutrient status in soils of Moodabidre TalukFigure 17Page 5
FULL TEXT Original article · reflowed for reading

Introduction

Soil fertility, compact-ability and erodibility are the elements of soil quality. Among these, the problem of decline in soil fertility endangers maximum productivity. Warren and Agnew (1988) described that of all the threats to sustainability, the threat due to soil fertility depletion is the most serious. Depending upon the cropping pattern, leaching, erosion etc., soil loses a considerable amount of nutrients every year. If cropping is continued over a period of time without nutrients being restored to the soil, its fertility will be reduced and crop yields will decline. Poor soil fertility conceives sparse plant cover, which promote erosion vulnerability. This happens because 90 percent of plant available Nitrogen (N) and Sulphur (S), 50-60 percent potassium (K), 25-30 percent phosphorus (P) and almost 70 percent of micronutrients reside in organic matter. Soil fertility is meant for highlighting the nutrient needs, based on fertility status of soils (and adverse soil conditions which need improvement) to realize good crop yields. Dakshina Kannada is one of the three coastal districts of the state with predominantly horticultural and industrial economy. The total geographical area is 4771 sq. kms of which 27% is covered by forests. The Topography of the District is undulating. The average altitude of the district is 30 meters above Mean Sea Level. The District is characterized by high rainfall (4000 mm mostly received during June to October) High temperature (Max-36.2 °C and Min 20.4 °C) and high humidity (84.5 to 96.5%). Soils are lateritic and acidic in nature. Cropping pattern shows that nearly one-third of the gross cropped area is under food grains and remaining under Plantation and horticultural crops like coconut, arecanut, black pepper, cashew etc. The district is a part of peninsular India located half way between Mumbai and Cape Cameron and is stretching 60 Kms. from North to South and 70 Kms. from East to West in the form of a low lying broken plateau from Western Ghats to Arabian Sea. In order to know information on present soil fertility status, this study was accompanied in different Taluks of Dakhsina Kannada district of coastal Karnataka.

Materials and Methods

The survey work was carried out to assess the availability of plant nutrients status in soils of Dakshina Kannada district of coastal Karnataka. Fifty representative soil samples from farmer fields were collected at different villages of each Taluka (Via. Bantwal, Belthanady, Puttur, Sullia, Kadaba and Moodabidri) during the month of April to May 2020 and later were analyzed in Soil and water testing laboratory of Krishi Vigyan Kendra, Dakshina Kannada. Electrical conductivity, pH, organic carbon, were determined by standard methods (Jackson 1973) [3] . Available nitrogen was estimated by alkaline permanganate method (Subbaiah and Asija, 1956) [13] . For available phosphorus determination, extraction was done using Brays extractant and then subsequent estimation by Jackson, (1973) [3] method. Available potassium was extracted using neutral normal ammonium acetate and measured with flame photometer (Jackson, 1973) [3] . Sulphur was extracted using 0.15 percent CaCl 2 solution and was made to react with BaCl 2 to form turbid solution of BaSO 4 . The intensity of turbidity was measured using spectrophotometer at a wavelength of 420 nm (Jackson, 1973) [3] . Exchangeable calcium and magnesium were determined using versenate (EDTA) titration method. Available micronutrients such as iron, copper, manganese and zinc were extracted using standard DTPA extract at pH 7.3 and the concentration was measured in an atomic absorption spectrophotometer (Lindsay and Norvell, 1978) [4] . Boron (Hot water extraction), particle size analysis by international pipette method and the percent base saturation was calculated by using following formula % Base saturation = Exchangeable Bases / CEC X 100

Results and Discussions

Results and Discussions

Physico-chemical properties

The data on particle size distribution of all the talukas of Dakshina Kannada were presented in above Table and is based the recorded data surface soil comprises more than 68 percent sand, 23 percent of clay and 9 percent of silt. As a result, these soils are texturally classified as sandy, sandy loam to sandy clay loam. As these areas receive high rainfall clay fraction is always subjected to illuviation process (Sahoo et al.1990) [7] . Soils of all the six Taluks were moderate to strongly acidic with highest average soil pH of 5.7 was recorded in Puttur Taluk (Fig. v) and lowest average pH of 4.9 was in soils of Sullia Taluk (Fig. ix). The acidic pH of the soil might be attributed mainly to the leaching of the bases due to the existing high rainfall conditions and to some extent due to the acidic parent materials. These soils are non-saline in nature (free of soluble salts) with average electrical conductivity ranges between 0.20-0.34 dSm -1 .

Cashew growing soils of Dakshina Kannada district of Karnataka are also high in organic carbon at the surface and low in sub-soils. It varied from 0.97 to 3.07 percent at the surface (Srinivasan et al. 2013) [11] . The average organic carbon content of the soils varied from 7.6 g kg -1 soil to 11.2 g kg -1 soil and was found to be high in all Taluks of the district. This is attributed to the addition of plant residues and farmyard manure to surface horizons. These results were justifiable with the studies of Harish Shenoy, 2019 [2] . Among soils of the different taluks studied cation exchange capacity was varied from 9.6-24.8 with mean value of 19.2 cmol (p + ) kg -1 . Further, percent base saturation was found low (7.0-32.0) with mean of 18.9 percent. This can be attributed to textural variations and difference in the status of organic matter (Rao 1992) [6] .

Available macronutrients

The status on available macronutrient contents of soils in different of Dakshina Kannada are depicted in Nitrogen status may due to the fact that the soil could retain only a limited quantity of mineralized Nitrogen and significant amount of Nitrogen loss through leaching and denitrification in these soils (Usha and Jose 1983) [14] . The available nitrogen was less than 280 kg ha -1 hence rated low (Srinivasamurthy et al., 1999) [10] . The available phosphorus content in soils of all Taluks averages varied from 16.2 to 21.8 kg ha -1 and was rated as low. Low available phosphorus of soils was due to the prevalence of heavy rainfall which leached all the base cations leaving mostly Fe and Al oxides, which fixes available phosphorus. Available potassium averages ranged from 121.2 to 272.0 kg ha - 1 and in most of the study area soils were with low to medium level of potassium. The highest average available K content was noticed in soils of Kadaba Taluk and lowest average in Bantwal Taluk. This could be attributed to more intensive weathering, release of labile K from organic residues and application of K fertilizers. Coarse textured and gravelly soils with deeper solum are particularly low in available potassium, possibly due to faster and deeper leaching and physico-chemical properties (Badrinath et al., 1986) [1] . Ratings for available potassium indicate that values less than 141 kg ha -1 are low 141to 336 kg ha -1 as medium as and more than 336 kg ha -1 as high (Srinivasamurthy et al., 1999) [10] . Similar results were reported in the studies of Singh et al., 2007 [9] . The average available sulphur in the soils varied from 7.74 to 9.51 mg kg -1 and most of the soils were very low in ratings. Belthangady and Bantwal Taluk soils had higher amount of available sulphur compared to other locations (Fig.

xiii to xviii).

Sidram Patil et al., 2017 [8] also reported similar results in their studies. Exchangeable calcium and magnesium in all the six Taluks of Dakshina Kannada were low and ranged from 1.27 to 1.82 Cmol (p + ) kg -1 and 0.59 to 0.99 Cmol (p + ) kg -1 respectively, this is due to the prevalence of excess and frequent rainfall in the study areas which leached most of the basic cations like calcium, magnesium, potassium and sodium from the surface soil to lower horizons.

Available micronutrients

The examination of the data on available micronutrients of the soils projected in Fig. xiii to xviii revealed that the DTPA extractable iron, manganese, zinc and copper content varied from deficiency to toxic level in soils of all the Talukas. The DTPA extractable Zn average ranged from 0.58 to 1.03 mg kg -1 soil as shown in Fig. xiii and xvi respectively. Considering 0.60 mg kg -1 as critical level for zinc deficiency (Lindsay and Norvell 1978) [4] , these soils could be classified as Sufficient in Zn except soils of Bantwal Taluk. The high content of available zinc in may be attributed to variable intensity of the pedogenic processes and complexing with organic matter which resulted in chelation of Zn. These observations are in accordance with the findings of Sidram Patil et al. (2017) [8] . Soils of all the Talukas were found to be sufficient in available copper (1.21 to 1.32 mg kg -1 ) as all the values were well above the critical limit proposed (0.20 mg kg -1 ) by Lindsay and Norvell (1978) [4] . The available Cu content was high which might be due to association with organic carbon and soil acidic pH. The DTPA extractable Fe content varied from 39.7 to 52.4 mg kg -1 soil. According to critical limit of 4.5 mg kg -1 (Lindsay and Norvell, 1978) [4] , the soils were rich in available iron. However, the higher DTPA-Fe in soils of all the Talukas might be due to accumulation of organic carbon in the surface horizons. The organic carbon due to its affinity to influence the suitability and availability of iron by chelating action might have protected the iron from oxidation and precipitation, which consequently increased the availability of iron (Prasad and Sakal, 1991) [5] .

Mean available Mn varied from 3.15 to 4.45 mg kg -1 soil and was found to be high in soils of all the Talukas. The highest average of 4.45 mg kg -1 was observed in soils of Kadaba Taluk and lowest average of 3.15 mg kg -1 was recorded in soils of Belthangady Taluk. Most of the soils of Dakshina Kannada were found low in available Boron (0.24 mg kg -1 ) hence there was extreme nut fall and nut cracking in some of the areca nut growing fields. These observations are in accordance with the findings of Srinivasan et al. (2013) [11] .

Conclusions

Fertility status of soils of Dakshina Kannada district of coastal Karnataka indicated that soils are low to medium in available N and available K and low in available P. Available Sulphur remained low in most soils. Among the exchangeable bases, exchangeable calcium was found to be high in most soils, followed by magnesium. With respect to micronutrients, iron and manganese contents were high, available copper was in sufficient range and available zinc was sufficient except in soils of Bantwal Taluk. Availability of boron was low in soils of all the Talukas of Dakshina Kannada. The deficient nutrients have to be restored through chemical fertilizers and/or organic manures to maintain soil health for efficient and sustainable crop production in these soils.

Figures and tables from the paper

Table 1. Ranges and means of physical, chemical and physicochemical
PropertiesRangeMean
pH (1: 2.5)4.90-5.705.13
EC (dSm-1)0.20-0.340.24
Organic carbon (g kg-1)7.6-11.20.91
Sand (%)58.32-77.468.32
Silt (%)6.37-14.839.88
Clay (%)20.5-31.7423.77
CEC (NH4OAc pH 7.0) (cmol (p+) kg-1)9.60-24.819.2
Base saturation (%)7.00-32.018.9
Available and exchangeable macronutrients
Nitrogen (kg ha-1)212.4-388.4242.7
Phosphorus (kg ha-1)16.2-21.819.95
Potassium (kg ha-1)121.2-272178.9
Sulphur (mg kg-1)7.74-9.518.48
Ex. calcium (cmol (p+) kg-1)1.27-1.821.62
Ex. magnesium (cmol (p+) kg-1)0.59-0.990.73
DTPA extractable micronutrients
Fe (mg kg-1)2.88-59.644.6
Mn (mg kg-1)3.15-4.453.89
Zn (mg kg-1)0.58-1.030.88
Cu (mg kg-1)1.21-1.321.24
B (mg kg-1)0.09-0.320.24

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Ranges and means of physical, chemical and physicochemical↗ Enlarge
Table 1
Ranges and means of physical, chemical and physicochemical

Ranges and means of physical, chemical and physicochemical

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Figure 1. pH, EC and Organic matter status of Bantwal Taluk
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Figure 1
pH, EC and Organic matter status of Bantwal Taluk

pH, EC and Organic matter status of Bantwal Taluk

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Figure 2. Primary nutrient status of Bantwal Taluk
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Figure 2
Primary nutrient status of Bantwal Taluk

Primary nutrient status of Bantwal Taluk

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Figure 3. pH, EC and Organic Carbon status in soils of Belthangady Taluk
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Figure 3
pH, EC and Organic Carbon status in soils of Belthangady Taluk

pH, EC and Organic Carbon status in soils of Belthangady Taluk

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Figure 4. Primary nutrient status in soils of Belthangady Taluk
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Figure 4
Primary nutrient status in soils of Belthangady Taluk

Primary nutrient status in soils of Belthangady Taluk

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Figure 5. pH, EC and Organic carbon status in soils of Puttur Taluk
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Figure 5
pH, EC and Organic carbon status in soils of Puttur Taluk

pH, EC and Organic carbon status in soils of Puttur Taluk

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Figure 6. Primary nutrient status in soils of Puttur Taluk
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Figure 6
Primary nutrient status in soils of Puttur Taluk

Primary nutrient status in soils of Puttur Taluk

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Figure 7. pH, EC and Organic carbon status in soils of Sullia Taluk
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Figure 7
pH, EC and Organic carbon status in soils of Sullia Taluk

pH, EC and Organic carbon status in soils of Sullia Taluk

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Figure 8. Primary nutrient status in soils of Sullia Taluk
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Figure 8
Primary nutrient status in soils of Sullia Taluk

Primary nutrient status in soils of Sullia Taluk

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Figure 9. pH, EC and Organic carbon status in soils of Moodabidri Taluk
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Figure 9
pH, EC and Organic carbon status in soils of Moodabidri Taluk

pH, EC and Organic carbon status in soils of Moodabidri Taluk

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Figure 10. Primary nutrient status in soils of Moodabidre Taluk
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Figure 10
Primary nutrient status in soils of Moodabidre Taluk

Primary nutrient status in soils of Moodabidre Taluk

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Figure 11. Secondary and Micronutrient status in soils of Bantwal Taluk
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Figure 11
Secondary and Micronutrient status in soils of Bantwal Taluk

Secondary and Micronutrient status in soils of Bantwal Taluk

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Figure 12. Secondary and Micronutrient status in soils of Belthangady
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Secondary and Micronutrient status in soils of Belthangady

Secondary and Micronutrient status in soils of Belthangady

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Figure 13. Secondary and Micronutrient status in soils of Puttur Taluk
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Secondary and Micronutrient status in soils of Puttur Taluk

Secondary and Micronutrient status in soils of Puttur Taluk

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Figure 14. Secondary and Micronutrient status in soils of Puttur Taluk
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Secondary and Micronutrient status in soils of Puttur Taluk

Secondary and Micronutrient status in soils of Puttur Taluk

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Figure 15. Secondary and Micronutrient status in soils of Kadaba Taluk
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Figure 15
Secondary and Micronutrient status in soils of Kadaba Taluk

Secondary and Micronutrient status in soils of Kadaba Taluk

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Figure 16. Secondary and Micronutrient status in soils of Sullia Taluk
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Figure 16
Secondary and Micronutrient status in soils of Sullia Taluk

Secondary and Micronutrient status in soils of Sullia Taluk

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Figure 17. Secondary and Micronutrient status in soils of Moodabidre Taluk
Secondary and Micronutrient status in soils of Moodabidre Taluk↗ Enlarge
Figure 17
Secondary and Micronutrient status in soils of Moodabidre Taluk

Secondary and Micronutrient status in soils of Moodabidre Taluk

Open full-size image ↗
Original paper figureSource PDF · page 5 ↗

References

12 in the original paper
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  8. Srinivasan R, Natarajan A, Anil Kumar KS, Kalaivannan D. Characterization of major cashew growing soils of Dakshina Kannada district of Karnataka. Agropedology. 2013;23(2):59-64.
  9. Srinivasan R, Natarajan A, Kalaivanan D, Anil Kumar KS. Soil fertility status of cashew growing soils of Dakshina Kannada district of coastal Karnataka. Journal of Plantation Crops. 2013;41(3):373-379.
  10. Subbaiah BV, Asija GL. A rapid procedure for estimation of available nitrogen in soils. Current Science. 1956;25:259260.
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