2.4.5 Available micr<strong>on</strong>utrients Sharma and Meelu (1975) found that applicati<strong>on</strong> <str<strong>on</strong>g>of</str<strong>on</strong>g> 15 t<strong>on</strong>nes FYM per ha to every crop <strong>in</strong>creased the available z<strong>in</strong>c <str<strong>on</strong>g>of</str<strong>on</strong>g> the <strong>soil</strong> from <strong>in</strong>itial status <str<strong>on</strong>g>of</str<strong>on</strong>g> 0.62 ppm to 1.09 ppm after six seas<strong>on</strong>s <str<strong>on</strong>g>of</str<strong>on</strong>g> cropp<strong>in</strong>g. In a l<strong>on</strong>g term field experiment, Anand Swarup and Ghosh (1980) observed that c<strong>on</strong>t<strong>in</strong>uous fertilizers applicati<strong>on</strong> enhanced available ir<strong>on</strong> c<strong>on</strong>tent <str<strong>on</strong>g>of</str<strong>on</strong>g> <strong>soil</strong> by two times. On the other hand, c<strong>on</strong>t<strong>in</strong>uous cropp<strong>in</strong>g for seven years decreased <strong>soil</strong> z<strong>in</strong>c c<strong>on</strong>tent as compared to fallow land, while c<strong>on</strong>t<strong>in</strong>uous phosphatic fertilizers applicati<strong>on</strong> reduced exchangeable Zn compared to c<strong>on</strong>trol plot as noticed by Subba Rao and Ghosh (1983). They also recorded enhanced Zn levels due to applicati<strong>on</strong> <str<strong>on</strong>g>of</str<strong>on</strong>g> <str<strong>on</strong>g>organic</str<strong>on</strong>g> manures. Prasad (1981) found that the natural complex<strong>in</strong>g agent such as <str<strong>on</strong>g>organic</str<strong>on</strong>g> manure was found to be important <strong>in</strong> <strong>in</strong>creas<strong>in</strong>g the availability <str<strong>on</strong>g>of</str<strong>on</strong>g> Zn and Fe to plants even under moderate or acute deficiency c<strong>on</strong>diti<strong>on</strong>. Nemath et al. (1987) observed that applicati<strong>on</strong> <str<strong>on</strong>g>of</str<strong>on</strong>g> FYM @ 37.4 to @ 69.4 t<strong>on</strong>nes per ha significantly <strong>in</strong>creased the ir<strong>on</strong> c<strong>on</strong>tent <str<strong>on</strong>g>of</str<strong>on</strong>g> <strong>soil</strong> after harvest <str<strong>on</strong>g>of</str<strong>on</strong>g> wheat crop. Rajeev Kumar et al. (1993) noticed that available Fe and Zn level <strong>in</strong> <strong>soil</strong> decl<strong>in</strong>ed <strong>in</strong> all treatments except FYM treated <strong>soil</strong>. Similarly, FYM applicati<strong>on</strong> for five years <strong>in</strong>creased the Zn c<strong>on</strong>tent <strong>in</strong> the Vertisols <str<strong>on</strong>g>of</str<strong>on</strong>g> Akola (Rao and Dakhore, 1994). Incorporati<strong>on</strong> <str<strong>on</strong>g>of</str<strong>on</strong>g> cott<strong>on</strong> stalks @ 5 t<strong>on</strong>nes per ha improved micr<strong>on</strong>utrients availability <strong>in</strong> sunflower-bengalgram cropp<strong>in</strong>g system (Quereshi et al., 1995). Similarly, micr<strong>on</strong>utrients availability significantly <strong>in</strong>creased by applicati<strong>on</strong> <str<strong>on</strong>g>of</str<strong>on</strong>g> vermicompost al<strong>on</strong>g with RDF than RDF al<strong>on</strong>e (Vasanthi and Kumaraswamy, 1996). Mathur (1997) reported that the availability <str<strong>on</strong>g>of</str<strong>on</strong>g> z<strong>in</strong>c and ir<strong>on</strong> <strong>in</strong> sandy loam <strong>soil</strong> decreased due to c<strong>on</strong>t<strong>in</strong>uous cropp<strong>in</strong>g <str<strong>on</strong>g>of</str<strong>on</strong>g> cott<strong>on</strong> wheat sequence. However, applicati<strong>on</strong> <str<strong>on</strong>g>of</str<strong>on</strong>g> FYM significantly <strong>in</strong>creased available z<strong>in</strong>c <str<strong>on</strong>g>of</str<strong>on</strong>g> <strong>soil</strong> compared to RDF and other treatments. Additi<strong>on</strong> <str<strong>on</strong>g>of</str<strong>on</strong>g> <str<strong>on</strong>g>organic</str<strong>on</strong>g> materials like FYM and sunnhemp <strong>in</strong>creased the availability <str<strong>on</strong>g>of</str<strong>on</strong>g> micr<strong>on</strong>utrients (Bellakki and Badanur, 1997). The <strong>in</strong>creased availability was attributed to enhanced microbial activity <strong>in</strong> the <strong>soil</strong> and the c<strong>on</strong>sequent release <str<strong>on</strong>g>of</str<strong>on</strong>g> complex <str<strong>on</strong>g>organic</str<strong>on</strong>g> substances that could have prevented micr<strong>on</strong>utrients from precipitati<strong>on</strong>, fixati<strong>on</strong>, oxidati<strong>on</strong> and leach<strong>in</strong>g and also additi<strong>on</strong> <str<strong>on</strong>g>of</str<strong>on</strong>g> these nutrients through <str<strong>on</strong>g>organic</str<strong>on</strong>g> sources. Sharma et al. (2000) observed that the DTPA-extractable micr<strong>on</strong>utrients like Zn, Fe, Mn and Cu enhanced significantly due to crop residues and FYM <strong>in</strong>corporati<strong>on</strong> compared to chemical fertilizers applicati<strong>on</strong>. 2.5 EFFECT OF ORGANIC MANURES ON BIOLOGICAL PROPERTIES OF SOIL 2.5.1 Dehydrogenase activity Biological oxidati<strong>on</strong> <str<strong>on</strong>g>of</str<strong>on</strong>g> <str<strong>on</strong>g>organic</str<strong>on</strong>g> compounds is generally a dehydrogenati<strong>on</strong> process and there are many dehydrogenases (enzymes catalyz<strong>in</strong>g dehydrogenati<strong>on</strong>), which are highly specific. Unlike the other enzymes, dehydrogenases do not accumulate extracellularly <strong>in</strong> <strong>soil</strong> and are directly related to viability <str<strong>on</strong>g>of</str<strong>on</strong>g> <strong>in</strong>tact cells. Hence, quantificati<strong>on</strong> has been recommended as a useful <strong>in</strong>dicator <str<strong>on</strong>g>of</str<strong>on</strong>g> biological activity <strong>in</strong> <strong>soil</strong> (Schaffer, 1993). Kavalappa (1989) recorded highest phosphate, dehydrogenase, urease and total biomass c<strong>on</strong>tents <strong>in</strong> the plots treated with FYM and chemical fertilizers.Kukreja et al. (1991) noticed that the total microbial biomass and dehydrogenase activity <str<strong>on</strong>g>of</str<strong>on</strong>g> <strong>soil</strong> were significantly <strong>in</strong>creased <strong>in</strong> the plots receiv<strong>in</strong>g FYM applicati<strong>on</strong> annually for 20 years. Sriramachandrasekharan et al. (1997) observed that green manures have potentials to ma<strong>in</strong>ta<strong>in</strong> higher dehydrogenase activity over farmyard manure, coir pith compost and paddy straw. Nature <str<strong>on</strong>g>of</str<strong>on</strong>g> the plant materials <strong>in</strong>corporated probably governs the type and number <str<strong>on</strong>g>of</str<strong>on</strong>g> microbial communities that can flourish under given c<strong>on</strong>diti<strong>on</strong>s. Baruah and Mishra (1984) noted that dehydrogenase activity was related to <strong>soil</strong> <str<strong>on</strong>g>organic</str<strong>on</strong>g> carb<strong>on</strong>, total N and phosphorus. Higher dehydrogenase activity was negatively correlated with aerobic bacterial count.
Chandravanshi (1998) noticed that microbial biomass, C c<strong>on</strong>tent and activities <str<strong>on</strong>g>of</str<strong>on</strong>g> dehydrogenase and phosphatase enzymes <strong>in</strong> the <strong>soil</strong> were <strong>in</strong>creased by the applicati<strong>on</strong> <str<strong>on</strong>g>of</str<strong>on</strong>g> FYM either al<strong>on</strong>e or <strong>in</strong> comb<strong>in</strong>ati<strong>on</strong> with NPK fertilizers.
- Page 1 and 2: IMPACT OF FARMERS’ ORGANIC FARMIN
- Page 3 and 4: Chapter No. I. INTRODUCTION CONTENT
- Page 5 and 6: I. INTRODUCTION Organic manures, in
- Page 7 and 8: II. REVIEW OF LITERATURE Organic ma
- Page 9 and 10: Sharma et al. (2000) observed a sig
- Page 11 and 12: 2.3.1 pH and EC Application <strong
- Page 13 and 14: Inclusion of <stro
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- Page 21 and 22: 3.3.2.2 Electrical conductivity Ele
- Page 23 and 24: IV. EXPERIMENTAL RESULTS The result
- Page 25 and 26: Table 3. Quantity of</stron
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- Page 29 and 30: Table 4 (Contd…..) Code Depth (cm
- Page 31 and 32: Table 5. Physical properties <stron
- Page 33 and 34: In sugarcane based cropping system
- Page 35 and 36: Table 8. Physical properties <stron
- Page 37 and 38: Table 9. Soil pH and EC values in d
- Page 39 and 40: Table 9 (Contd…..) Code Depth (cm
- Page 41 and 42: Table 11. Organic carbon and cation
- Page 43 and 44: Table 13. Organic carbon and cation
- Page 45 and 46: soils, respectively. The highest in
- Page 47 and 48: Table 14 (Contd…..) Code Depth (c
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- Page 51 and 52: Table 16. Available potassium (kg K
- Page 53 and 54: Table 17. Available sulphur (kg S/h
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- Page 57 and 58: Table 18. DTPA-extractable zinc and
- Page 59 and 60: Table 20. DTPA-extractable zinc and
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- Page 63 and 64: Table 23. DTPA-extractable manganes
- Page 65 and 66: Table 25. DTPA-extractable manganes
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Table 26. Dehydrogenase activity (
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In kharif jowar based cropping syst
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5.2 EFFECT OF ORGANIC FARMING ON PH
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farmer under kharif jowar (10.90%),
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consequent release of</stro
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VII. REFERENCES ACHARYA, C. L., BIS
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CHENKAI, 1993, Vetiver as a live bu
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LAL, J. K., MISHRA, B. AND SARKAR,
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RATHOD, V. E., SAGARE, B. N., RAVAN
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TANDON, H. L. S., 1983, Fertilizer