Research Article

Soil Nutrient Analysis Underneath Grewia optiva Population

H. P. Sankhyan, Jyoti Dhiman, Krishan Chand, Prachi Karishma and Bhupender Negi

  • Page No:  645 - 654
  • Published online: 30 Dec 2021
  • DOI : HTTPS://DOI.ORG/10.23910/1.2021.2643b

  • Abstract
  •  sankhyanhp@gmail.com

The present study was conducted during May and November, 2019 and 2020 and here we quantify the impact of soil nutrient variation on the population growth of Grewia optiva Drummond of different districts with variable climate and heterogeneous soils. The impacts on growth parameters (tree height, crown spread, leaf traits, fruit dimensions) of selected populations of Grewia optiva Drummond statistically analyzed using ANOVA and Pearson correlation coefficient. Five composite soil samples were taken at 15–30 cm depth, on seven selected districts of Himachal Pradesh viz., total 35 samples were analyzed for physiochemical properties. Soil of Mandi district registered with acidic pH as compared to soil pH of other districts. There was significant difference in pH, OC, EC, N, P, K and in Bulk density within selected population of each district. pH range of moderately acidic to moderately alkaline (according to standard soil classification) founded best for growth of this species. There was highly positive correlation observed between Nitrogen and leaf area (0.33), Phosphorus and leaf area (0.45). 100 leaf fresh weight showed highly positive correlation with Nitrogen (0.37) and organic carbon (0.39). 100 leaf dry weight showed highly positive correlation with Nitrogen and Organic Carbon. Crown spread showed highly positive correlation with Organic carbon (0.29), Nitrogen (0.38) and with Phosphorus (0.30). Moderately Positive correlation observed between Potassium and 100 fruit dry weight (0.15).50% of soil texture observed as sandy loamy and sandy clay loamy. 

Keywords :   Fodder, Grewia optiva, growth, macronutrient, plant community, soil

  • Introduction

    Grewia optiva, commonly known as Biul/Bihul/Bhimal, belongs to family Tiliaceae. This species is preferred by hilly farmers of the Uttarakhand, Himachal Pradesh, Nepal etc., for its attributes like palatability, faster growth, ease of propagation and forage yield (Mukherjee et al., 2018). It provides fodder during lean season, when no alternate to green fodder is available. (Katoch et al., 2017). It has over 70 percent potential DM digestibility and effective degradability (56.7 Per cent) which makes it superior energy source for ruminants (Singh et al., 1989). The genus Grewia consists of some 150 species in world, out of which 42 species are found in Indian subcontinent (Bhagta et al., 2021).

    Soil consists of definite chemical, physical, mineralogical and biological properties, which provides a medium for plant growth (Thakre et al., 2012).  The knowledge of physiochemical properties viz; organic carbon, available Nitrogen (N), Phosphorus (P25), Potassium (K2O), pH, electrical conductivity, soil texture and bulk density of soil is also important to determine the available nutrient status in soil and to develop specific fertilizer recommendations. (Sumithra et al., 2013). As pH is a good indicator of the balance of available nutrients in the soil whereas, Electrical Conductivity can almost be viewed as the quantity of available nutrients in the soil. (Smith and Doran, 1996). The response of trees to increasing atmospheric CO2 concentrations is often mediated by the availability of nutrients in the soil (Schleppi et al., 2019). Whether terrestrial ecosystems, forests, crop land trees are sources or sinks for CO2 and their growth will ultimately depend on interactions of the C cycle with the cycles of nutrients, especially nitrogen (N) and phosphorus (P) (Ellsworth et al., 2017). An increased production of exoenzymes has been found in several studies with CO2 enrichment, and this effect has depended on the availability of N in the soil (Drake et al., 2013, Meier et al., 2017, Ochoa-Hueso et al., 2017). Nitrogen (N) is one of the most important biological elements for plants, agricultural crops and forest trees, because it is a component of amino acids, proteins, genetic materials, pigments, and other key organic molecules (Chen et al., 2014, Ji et al., 2015, Liu et al., 2018). N has an irreplaceable role in organ construction, material metabolism, fruit yield, and the quality formation of fruit trees (Bai et al., 2016). Soil nitrogen (N) deficiencies can affect the photosynthetic N-use efficiency (PNUE), mesophyll conductance (gm), and leaf N allocation (Tang et al., 2019). Potassium (K) is used for flowering purpose, it is also required for building of protein, photosynthesis, fruit quality and reduction of diseases (Valente et al., 2012). Potassium is an activator of dozens of important enzymes, such as protein synthesis, sugar transport, N and C metabolism, and photosynthesis. It plays an important role in the formation of yield and quality improvement (Marschner, 2012, Oosterhuis et al., 2014). Potassium has strong mobility in plants and plays an important role in regulating cell osmotic pressure and balancing the cations and anions in the cytoplasm (Hu et al., 2016a). Phosphorus (P) is also an essential plant nutrient for various tree growth functions ( Jonard et al. 2015). Plants take up Phosphorus in its inorganic form as phosphate (Becquer et al., 2014). Phosphorus limitation decreases the efficiency of plant respiration (Jiang et al., 2019) and night respiration may increase along the N/P ratio. Therefore, considering the importance of the physiochemical properties of the soil mentioned above, the present study was carried out to perform a correlation and nutritional analysis of the soil under the populations of Grewia optiva Drummond in Himachal Pradesh.


  • Materials and Methods

    2.1.  Study area and sampling station selection

    The present study on analysis of physiochemical characteristics of soil was carried out during May and November, 2019 and 2020 in seven districts of Himachal Pradesh i.e., Kangra, Mandi, Bilaspur, Solan, Sirmour, Una and Hamirpur, keeping in view the rich genetic diversity and phenotypically superior plant populations of Grewia optiva. Total thirty-five population (five population in each district) were selected. In each population six superior trees of 20 cm–30 cm diameter class were marked. The soil samples were collected from 15 cm–30 cm depth underneath the selected populations of Grewia optiva Drummond. In each collection 35 composite soil samples (each a composite of six cores) were taken. The soil samples were collected in two consecutive years 2019 and 2020, twice in year i.e., in the month of May and November. In 2019, first soil sample was collected during the Month of May, when this species was in leafing and flowering stage and second sample was taken at six months interval in the month of November, when the species was in the seed ripening and fodder lopping stage. Similarly, in the year 2020, two consecutive samples were collected in month of May and November from the same selected sites and depth (15 cm–30 cm) respectively, from all thirty five populations. Thus, a total of four samples were taken in two consecutive years from each population and their data was statistically analysed separately for each interval. The pooled data from two years presented for statistical analysis and evaluation in the year 2021 under the present investigation. The morphometric traits of these selected superior trees have been recorded simultaneously. Further the correlation established between physiochemical characteristics of soil and morphometric traits of selected populations.

    2.2.  Sampling procedure

    In order to collect soil samples (15 cm–30 cm depth) first removed grasses, litter and other plant residues from soil surface and collect soil samples by using soil collection tools. In each case, a triangular block was marked and soil samples were collected in plastic bags, which were sealed, and labelled properly.Collected soil were air dried, lightly grounded and sieved to remove coarse particles (≥2mm) to ensure homogeneity. Mineral soil <2mm was subsampled in the field (approx. 150 g) and transported to laboratory of Soil- science, University of Horticulture and Forestry, Nauni, Solan (HP) for further analysis of morphological (soil texture), physiochemical (Bulk density, pH, EC) and other available macronutrients (N, P, K) on the basis of standard methods (Table 1).


    2.3.  Analysis

    Analysis of variance (ANOVA) and Pearson correlation coefficient (p<0.05) used to find correlation between physiochemical properties of soil and morphological characteristics of selected population of Grewia optiva which had been recorded simultaneously. Standard Soil Classification (Iram and Khan, 2018) (Table 2) has been used for the comparative analysis of different parameters of soil.


  • Results and Discussion

    There was significant difference was observed in pH, OC, EC, bulk density and in macronutrients (N, P, K ) within selected population of each district. Macro and Micro nutrients of the soil are equally important for growth and development of the plants but in the present investigation only the major macronutrients viz; N, P, K have been analyzed.

    3.1.  pH

    pH of the soil at depth of 15–30 cm of district Solan (Table 3) ranged from 6.70–7.66 with mean value of 7.24, of district Una ranged from 6.60–7.80 with mean value of 7.14, of Sirmour district ranged from 6.76 –7.52 with mean value 7.05, of Hamirpur district ranged from 7.10–7.30 with mean value 7.16, Kangra district ranged from 6.01–7.65 with mean value of 6.84, of Mandi district ranged 5.1 to 6.3 with mean value 5.76 and of Bilaspur district ranged from 5.92 to 7.68 with mean value 7.12.  The lowest pH of 5.1 was reported beneath Balt population of Mandi district, whereas highest beneath Nawami population of Una district. In this study pH range of moderately acidic to moderately alkaline reported best for the growth of this species.  100 leaf fresh weight, tree height, tree diameter, crown spread, no. of secondary branches and 100 fresh fruit weight showed positive correlation with the pH (Table 4, Figure 1). The most important role of pH is the control of nutrients solubility in soil. Nutrient availability usually decreases with increasing pH (Kazem et al., 2012).


    3.2.  Electrical conductivity (dSm-1) (EC)

     Electrical conductivity for the soil of district Solan (Table 3)  ranged from 0.17–0.33 (dSm-1) with mean value of 0.24 (dSm-1), of district Una ranged from 0.11–0.22 (dSm-1) with mean value of 0.11 (dSm-1), District Sirmour 0.26–0.54 (dSm-1) with mean value of 0.42 (dSm-1), of district Hamirpur 0.47–1.32 (dSm-1) with mean value 0.85 (dSm-1), District Kangra ranged between 0.11–0.19 (dSm-1) with mean value 0.14, of district mandi ranged 0.16–0.21 with mean value 0.16 (dSm-1) and of  district Bilaspur 0.12–0.81 (dSm-1) with mean value 0.39 (dSm-1). The highest EC 1.32 (dSm-1) was reported beneath Bhaleth population of Hamirpur district, whereas minimum 0.10 (dSm-1) beneath old Kangra population. 100 leaf fresh weight, Tree diameter and crown spread showed moderately positive correlation with EC (Table 4, Figure 1). EC values affects uptake of nutrients by the tree. Very high or low EC decreases plants fresh weight (FW) and dry weight (DW), leaf size, leaf water content, leaf net photosynthetic rate (Pn), stomatal conductance (Gs), transpiration rate (Tr), (Sonneveld and De Kreij, 1996). In present study EC recorded above 0.6 (dSm-1) up to 1.32 (dSm-1) (Table 3) lies in range of non-saline soil (NRCS–USDA,1999) which was recorded favorable for growth of this species.

    3.3.  Organic carbon (g kg-1) (OC)

    Organic carbon for the soil of district Solan (Table 3) ranged from 3.50–10.70 (g kg-1) or 0.3–1.07 % with mean value of 7.1 (g kg-1)/0.7 %, of district Una ranged from 10.02–16.09 (g kg-1) or 1.02–1.609 % with mean value of 12.31 (g kg-1) or 1.23 %, District Sirmour 12.6–19.05 (g kg-1) or 1.26–1.905 % with mean value of 15.78 (g kg-1)/ 1.57%, of district Hamirpur 17.21–27.25 (g kg-1) or 1.72–2.72% with mean value of 23.28 (g kg-1)/2.3%, District Kangra ranged between 7.05–14.10 (g kg-1) or 0.70–1.41%  with mean value 10.47 (g kg-1)/1.04%, of district Mandi ranged 1.01–2.70 (g kg-1) or 0.10–0.27% with mean value 1.78  (g kg-1)/0.17%  and of  district Bilaspur 15.20–27.50 (g kg-1) or 1.52–2.75%. The highest organic carbon recorded in soil of Barthin Population of Bilaspur district, whereas lowest found in Gangal Population of Mandi district. 100 leaf fresh weight, 100 leaf dry weight, and crown spread showed highly positive correlation with OC, whereas leaf area, tree diameter and tree height showed negative correlation with it (Table 4, Figure 1). Soil organic carbon is a natural resource for the sustainable development of human society and a key foundation for sustainable forestry development (Panet al., 2015). It plays an important role in the formation and conservation of soil structure, soil nutrient cycling and soil biodiversity.

    3.4.  Nitrogen (kg ha-1)

    Nitrogen underneath district Solan (Table 3) population ranged from 270.79–343.92 (kg ha-1) with mean value of 303.15 (kg ha-1), of district Una ranged from 280.18–360.60 (kg ha-1) with mean value of 307.60 (kg ha-1), District Sirmour 343.79–379.51 (kg ha-1)  with mean value of 365.48 (kg ha-1), of district Hamirpur 344.91–380.33 (kg ha-1) with mean value of  369.63 (kg ha-1), District Kangra ranged between 272.83–363.77 (kg ha-1) with mean value 306.07 (kg ha-1), of district Mandi ranged  between 115–231 (kg ha-1) with mean value 149.5 (kg ha-1) and of  district Bilaspur ranged between 362.70–419.20(kg ha-1) with mean value 382.18 (kg ha-1). The highest Nitrogen recorded in soil of Barthin Population of Bilaspur district, whereas lowest found underneath Bagla Population of Mandi district. Leaf area, 100 leaf fresh weight, 100 leaf dry weight, crown spread, no. of primary branches and 100 fruit fresh weight showed positive correlation with the available nitrogen in the soil (Table 4, fig 1). Similar results recorded in Douglas-fir by (Brix and Ebell,1969), which revealed that fertilization with Nitrogen increased basal area increment, stem height, and branch length, leaf area, leaf length-width, the no. of leaves per shoot increased markedly. (Wang et al.,2012) reported increased specific leaf area (SLA) and leaf area index (LAI) with N fertilization. A study on Fagus sylvatica by (Meier and Leuschner, 2008) reported positive effects on leaf area and LAI in forests with increased in nitrogen availability.

    3.5.  Phasphorus (kg ha-1) 

    Phosphorus content in soil of district Solan (Table 3) ranged from 14.93–33.60  (kg ha-1) with mean value of 24.19 (kg ha-1), of district Una ranged from 25.60–56.89 (kg ha-1) with mean value of 38.47 (kg ha-1), District Sirmour (kg ha-1) ranged between 33.06–63.96 (kg ha-1) with mean value of 47.84 (kg ha-1), of district Hamirpur 34.70–43.60 (kg ha-1) with mean value of  38.35 (kg ha-1), District Kangra ranged between 24.64–53.76 (kg ha-1) with mean value 37.18 (kg ha-1), of district Mandi ranged  between 18.8–37.5 (kg ha-1) with mean value 29.28 (kg ha-1) and of  district Bilaspur ranged between 37.20–45.62 (kg ha-1) with mean value 41.62 (kg ha-1). The highest available phosphorus recorded in soil of Badon Population of Sirmour district, whereas lowest underneath Bharnoi Population of Mandi district. Leaf area and crown spread showed positive correlation (Table 4, fig 1) with the available phosphorus in soil. In a similar study by (Herbert and Fownes, 1995) in native  Metrosideros polymorpha forest showed that increased available phosphorus promoted an increase in photosynthetic area which led to increased tree growth.

    3.6.  Potassium (kg ha-1)  

    Potassium content in soil of district Solan (Table 3) ranged from 212.80–489.81  (kg ha-1) with mean value of 337.24 (kg ha-1), of district Una ranged from 285.38–477.21 (kg ha-1) with mean value of 350.45 (kg ha-1), District Sirmour (kg ha-1) ranged between 285.96–512.46  (kg ha-1) with mean value of 398.62 (kg ha-1), of district Hamirpur 161.30–272.10 (kg ha-1) with mean value of  229.35 (kg ha-1), District Kangra ranged between 283.36–577.92 (kg ha-1) with mean value 368.70 (kg ha-1), of district Mandi ranged  between 182–480 (kg ha-1) with mean value 330 (kg ha-1) and of  district Bilaspur ranged between 213.40–328.80 (kg ha-1) with mean value 267.30 (kg ha-1). The highest available Pottasium recorded underneath Balla of Population of Kangra district, whereas lowest Bharnoi Population of Mandi district. Leaf area showed moderately positive correlation with the available potassium in the soil (Table 4, figure 1). A similar study in Eucalyptus grandis by (Battie-Laclau et al., 2013) reported that K and Na applications enhanced tree leaf area by increasing both leaf longevity and the mean area of individual leaves.

    3.7.  Soil Texture

    Soil of different texture were founded underneath populations of different districts (Table 3) viz; 50% of soil texture observed as sandy loamy and sandy clay loamy followed by clay loamy (20%), gravelly loamy (10%), loamy (10%) and remaining silty clay loamy (5%) and silty loam (5%). The tree has a capacity to grow in almost any type of soil but sandy loam with proper moisture is most suitable for its proper growth. (Singh et al., 2018).

    3.8.  Bulk density (BD) 

    Bulk density underneath  soil of district Solan populations  (Table 3) ranged from 0.99–1.17 with mean value of 1.11,  of district Una ranged from 1.04–1.21 with mean value of  1.13,  district Sirmour  ranged between 1.15–1.70 with mean value of 1.31, of district Hamirpur 1.11–1.46  with mean value of  1.14,  District Kangra ranged between 1.08–1.22 with mean value 1.15, of district Mandi ranged  between 1.01–1.38 with mean value 1.20 and of  district Bilaspur ranged between 1.08–1.33 with mean value 1.18 . The highest BD recorded underneath Machair Population of Sirmour district, whereas lowest in soil of Neri Kalan population of Solan district. No. of primary branches showed highly positive correlation with the BD, no. of secondary branches, 100 fruit dry weight showed moderately positive correlation with the BD (Table 4, Figure 1). The bulk density depends on compaction, consolidation of the soil but it is negatively correlated to the organic content (Micheni et al., 2004).

    Analysis of physiochemical characteristics of soil underneath selected Grewia optiva Drummond populations of Himachal Pradesh concluded that this species can grow in moderately acidic to moderately alkaline pH. Soil which was rich in OC gave more growth in leaf area, 100 leaf dry weight and in crown spread. Increase in available nitrogen positively increase vegetative growth of the trees. Available phosphorus was present in less and in medium concentration in all the soil samples except Badon population of Sirmour district. Whereas potassium was present in medium, average, better and in more than sufficient amount underneath selected populations at different districts but the soil underneath Bhaleth population of Hamirpur district found less in available potassium. Nitrogen is considered to be the most important nutrient, and plants absorb more nitrogen than any other element. Nitrogen is essential in the formation of protein, and protein makes up much of the tissues of most living things. Increase in available phosphorus affected positively leaf area, crown spread, no. of branches and fruit. Phosphorus, is linked to a plant’s ability to use and store energy, including the process of photosynthesis. It’s also needed to help plants grow and develop normally (Yosuf et al., 2017). Potassium is known to affect cell division, cell permeability formation of carbohydrates, translocation of sugars, various enzyme actions and resistance of some plants to certain diseases (Miller and Turk, 2002). It helps strengthen plants’ abilities to resist disease and plays an important role in increasing crop yields and overall quality. Potassium also protects the plant when the weather is cold or dry, strengthening its root system and preventing wilt. Therefore Nitrogen (promotes leaf growth), Phosphorus (root, flower, and fruit), and Potassium supports stem and root growth and protein analysis. Variability observed in soil texture, which concluded that this species can grow on variety of soil but maximum growth observed under Sandy loam soil. Variability in soil texture may contribute to the variation in nutrient storage and availability, water retention and transport and binding and stability of soil aggregates. Soil texture directly or indirectly influences soil functions such as soil erosion, water availability (Adhikari et al., 2009).


  • Conclusion

    Study concludes that this species can grow in moderately acidic to moderately alkaline pH. Thirty biologically screened populations found good in soil fertility status under crop land situation for the production of quality planting material except populations of Mandi district. Fifty percent of soil texture examined as sandy loamy and sandy clay loamy underneath these populations which favours the growth of this species. Screened populations under study have been found as best seed sources to obtain highly nutritive strains.


  • Acknowledgement

    The authors are very thankful to National Mission on Himalayan Studies (NMHS) G.B. Pant National Institute of Himalayan Environment and Sustainable Development (GBPNIHESD), Kosi–Katarmal, Almora-263643, Uttarakhand, India under the Ministry of Environment Forest & Climate Change, Govt. of India, Jorbhag Road, New Delhi–110003 for funding this project entitled “Biological Screening, Conservation and Establishment of Gene Bank of Grewia optiva Drummond (Beul).” to this department for undertaking this present study.


  • Reference
  • Adhikari, K., Guadagnini, A., Toth, G., Hermann, T., 2009. Geostatistical analysis of surface soil texture from Zala County in western Hungary. International Symposium on Environment, Energy and Water in Nepal: Recent Researches and Direction for Future, 219–224.

    Bai, L., Deng, H., Zhang, X., Yu, X., Li, Y., 2016. Gibberellin Is Involved in Inhibition of Cucumber Growth and Nitrogen Uptake at Suboptimal Root-Zone Temperatures. PLoS One 11(5), e0156188. https://doi.org/10.1371/journal.pone.0156188

    Battie-Laclau, P., Laclau, J.P., Piccolo,  M.C., Arenque Beri , C., Mietton, L., Muniz , M.R., Meille- Buckeridge, M.S., Nouvellon, Y., Ranger, J., Bouillet, J.P.,2013. Influence of Potassium and Sodium Nutrition on Leaf Area Components in Eucalyptus grandis Trees.  Plant and Soil 371, 19–35.

    Becquer, A., Trap, J., Irshad, U., Ali, M.A., Claude, P., 2014. From soil to plant, the journey of P through trophic relationships and ectomycorrhizal association. Frontiers in Plant Science 5, 548. doi: 10.3389/fpls.2014.00548

    Bhagta. S., Thakur, P., Sharma D., 2021. Genetic divergence study in Grewia optiva through Quantitative and Molecular markers. International Journal of Economic Plants, 029-033. DOI: HTTPS://DOI.ORG/10.23910/2/2020.0396

    Brix, H., Ebell, L.F., 1969. Effects of Nitrogen fertilization on Growth, leaf area, and photosynthesis rate in Douglas-Fir. Forest Sciences 15, 189-196.

    Chen, L.H., Dong, T.F., Duan, B.L., 2014. Sex-specific carbon and nitrogen partitioning under N deposition in Populus cathayana. Trees 28, 793–806.https://doi.org/10.1007/s00468-014-0992-3.

    Drake, J.E., Gallet-Budynek, A., Hofmockel, K.S., Bernhardt, E.S., Billings, S.A., Jackson, R.B., 2013. Increases in the flux of carbon belowground stimulate nitrogen uptake and sustain the long-term enhancement of forest productivity under elevated CO2. Ecology Letters 14, 349–357. doi: 10.1111/j.1461-0248.2011. 01593.x

    Ellsworth, D.S., Anderson, I.C., Crous, K.Y., Cooke, J., Drake, J.E., Gherlenda, A.N., 2017. Elevated CO2 does not increase Eucalypt forest productivity on a low-phosphorus soil. Nature Climate Change 7, 279–283. doi: 10.1038/nclimate3235

    Herbert, D.A., Fownes, J.H., 1995. Phosphorus limitation of forest leaf area and net primary production on a highly weathered soil. Biogeochemistry29, 223-235.

    Hu, W., Zhao, W., Yang, J., Oosterhuis, D.M., Loka, D.A., Zhou, Z., 2016a. Relationship between potassium fertilization and nitrogen metabolism in the leaf subtending the cotton (Gossypium hirsutum L.) boll during the boll development stage. Plant Physiology and Biochemistry 101, 113–123. doi: 10.1016/j.plaphy.2016.01.019

    Iram, A., Khan, T., 2018. Analysis of soil quality using physico-chemical parameters with special emphasis on fluoride from selected sites of sawai Madhopur Tehsil, ajasthan. International Journal of Environmental Sciences and Natural Resources 12(5), 555847

    Jackson, M.L., 1973. Soil Chemical Analysis. Prentice Hall of India (Pvt.) Ltd., New Delhi. 85, 251–252.

    Ji, D.H., Mao, Q.Z., Watanabe, Y., Kitao, M., Kitaoka, S., 2015. Effect of nitrogen loading on the growth and photosynthetic responses of Japanese larch seedlings grown under different light regimes. Journal of Agricultural Meteorology 71, 232–238. https://doi.org/10.2480/ agrmet. D-14-00027

    Jiang, M., Caldararu, S., Zaehle, S., Ellsworth, D.S., Medlyn, B.E., 2019. Towards a more physiological representation of vegetation phosphorus processes in land surface models. New Phytologist 222, 1223–1229. doi: 10.1111/nph.15688

    Jonard, M., Furst, A., Verstraeten, A., 2015. Tree mineral nutrition is deteriorating in Europe. Global Change Biology 21, 418–430.

    Katoch, R., Singh, S.K., Tripath, A., Kumar, N., 2017. Effect of seasonal variation in biochemical composition of leaves of fodder trees prevalent in the mid-hill region of Himachal Pradesh. Range Management and Agroforestry38, 234–240.

    Kazem, H., Tayebeh, M., Farani, S., Jamaati-e-Somarin, 2012. Effect of elemental sulphur and compost on pH, electrical conductivity and phosphorus availability of one clay soil. African Journal of Biotechnology 11, 1425-1432.

    Liu, N., Wang, J., Guo, Q., Wu, S., Rao, X., Cai, X., Lin, Z., 2018. Alterations in leaf nitrogen metabolism indicated the structural changes of subtropical forest by canopy addition of nitrogen. Ecotoxicology and Environmental Safety 160, 134–143. https://doi.org/10.1016/j.ecoenv.2018.05.037 (2018)

    Marschner, H., 2012. Marschner’s Mineral Nutrition of Higher Plants. Cambridge, MA: Academic press.

    Meier, I.C., Finzi, A.C., Phillips, R.P., 2017. Root exudates increase N availability by stimulating microbial turnover of fast-cycling N pools. Soil Biology and Biochemistry 106, 119–128. doi: 10.1016/j.soilbio.2016.12.004

    Meier, I.C., Leuschner, C.,2008. Leaf Size and Leaf Area Index in Fagus sylvatica Forests: Competing Effects of Precipitation, Temperature, and Nitrogen Availability. Ecosystem  11, 655–669

    Merwin, H.D., Peech, M.,1951. Exchangeability of soil potassium in the sand, silt and clay fractions as influenced by the nature of the complementary exchangeable cation. Soil Science Society of America Journal. 15, 125–128.

    Micheni, A., Kihanda, F., Irungu, J., 2004. Soil organic matter (SOM): The basis for improved crop production in arid and semi-arid climate of eastern Kenya. In Managing Nutrient Cycles to Sustain Soil Fertility in Sub-Saharan Africa; Bationo, A., Ed.; Academy Science Publisher: Nairobi, Kenya, 608

    Miller, C., Turk, L.M.,2002. Fundamentals of soil science Biotech. Books, 1123/74, Trinagar, Delhi, India pp. 157

    Mukherjee, A., Modal, T., Bist, J.K., Pattanayak, A., 2018. Farmer’s preference of fodder trees in mid hills of Uttarakhand: A comprehensive ranking using analytical hierarchy process. Range Management and Agroforestry 39, 115–120.

    NRSC-USDA,1999.  Soil Taxonomy - A Basic System of Soil Classification for Making and Interpreting Soil Surveys. Agriculture Handbook. No., 436.

    Ochoa-Hueso, R., Hughes, J., Delgado-Baquerizo, M., Drake, J.E., Tjoelker, M.G., Pineiro, J., 2017. Rhizosphere-driven increase in nitrogen and phosphorus availability under elevated atmospheric CO2 in a mature Eucalyptus woodland. Plant and Soil 416, 283–295. doi: 10.1007/s11104-017-3212-2

    Olsen, S.R., Cole, C.V., Watanable, F.S., Dean, L.A.,1954. Estimation of available phosphorus in soil by extraction with NaHCO­3, USDA Circular, US Washington. 939, 19p.

    Oosterhuis, D., Loka, D., Kawakami, E., Pettigrew, W., 2014. The physiology of potassium in crop production. Advances in Agronomy 126, 203–234. doi: 10.1016/B978-0-12-800132-5.00003-1

    Pan, G., Lu, H., Li, L., Zhang, J., Zhang, X.,2015. Soil Carbon Sequestration with Bioactivity: A New Emerging Frontier for Sustainable Soil Management. Advances in Earth Science30, 940–951.

    Schleppi, P., Korner, C., Klein, T., 2019. Increased Nitrogen availability in the soil under mature Picea abies trees exposed to elevated Co2 concentrations. Frontiers in Forests and Global Change 2, 59.   

    Singh, B., Makkar, P.S., Negi, S.S., 1989. Rate and extent of digestion and potentially digestible dry matter and cell wall of various tree leaves. Journal of Dairy Science72, 3233–3239.

    Singh, C., Singh, R., Himshikha, 2018. Grewia optiva (Drumm. Ex Burr)–A Multi-Purpose Tree Under Agroforestry in Sub-Tropical Region of Western Himalaya. Journal of Tree Sciences 37, 36–43.

    Smith, J.L., Doran, J.W.,1996. Measurement and use of pH and electrical conductivity for soil quality analysis. Methods for assessing soil quality, 169–185.

    Sonneveld, C., De Kreij, C.,1996. Response of cucumber (Cucumis sativus L.) to an unequal distribution of salts in the root environment. Plant and Soil 209, 45–56.

    Subbaiah, B.V., Asija, G.L.,1956. A rapid method for the estimation of available nitrogen in soil. Current Science25, 258–260.

    Sumithra, S., Ankalaiah, C., Rao, D., Yamuna, R.T., 2013. A case study on physico-chemical characteristics of soil around industrial and agricultural area of yerraguntla, kadapa district, AP, India. International Journal Geology Earth and Environmental Sciences 3, 28–34.

    Tang, J., Sun, B., Cheng, R., Shi, Z., Luo D., Liu, S., Centritto, 2019. Effects of soil nitrogen (N) deficiency on photosynthetic N-use efficiency in N-fixing and non-N-fixing tree seedlings in subtropical China. Scientific Reports 9, 4604 https://doi.org/10.1038/s41598-019-41035-1

    Thakre, Y.G., Choudhary, M.D., Raut, R.D.,2012. Physicochemical Characterization of Red and Black Soils of Wardha Region. International Journal of Chemical and Physical Sciences 1, 60–66.

    Valente, D.S.M., Queiroz, D.M., Pinto, F., Santos, N.T., Santos, F.L., 2012. Definition of Management Zones in Coffee Production Fields Based on Apparent Soil Electrical Conductivity. Scientia Agricola 69, 173–179.

    Walkley, A.J., Black, I.A.,1934.  Estimation of soil organic carbon by the chromic acid titration method. Soil Science 37, 29–38.

    Wang, D., Mathew, W.M., Jindong, S., Xiaohui, F., Fernando, M., Dokyoung, L., Michael C.,2012. Impact of nitrogen allocation on growth and photosynthesis of Miscanthus (Miscanthus×giganteus) GCB  Bioenergy4, 688–697.

    Yosuf, M., Li J., Lu J., Ren, T., Cong R., Fahad, S., Li, X., 2017. Effects of fertilization on crop production and nutrient-supplying capacity under rice-oilseed rape rotation system. Scientific reports7, 1–9.


Cite

1.
Sankhyan HP, Dhiman J, Ch K, , Karishma P, Negi B. Soil Nutrient Analysis Underneath Grewia optiva Population IJBSM [Internet]. 30Dec.2021[cited 8Feb.2022];12(1):645-654. Available from: http://www.pphouse.org/ijbsm-article-details.php?article=1537

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