Soil quality parameters
Application of organic manures and inorganic NPK fertilizers showed marked difference on physico-chemical properties of soil (pH and EC) at tillering, panicle initiation and harvest stage of rice. At all growth stages of rice, the highest available nitrogen, phosphorus, potassium, micronutrients (Fe, Mn, Zn and Cu), urease, dehydrogenase and microbial population (bacteria, fungi and actinomycetes) in soil were recorded with application of In-organics+Dhaincha @ 10 t ha
-1. Changes in soil physical, chemical and biological parameters were monitored at the end of every year and results at the end of fifth year are presented in Tables 1 to 4. There was a significant improvement in soil physical (bulk density and water stable aggregates), fertility (organic carbon and available N, P
2O
5 and K
2O) and biological properties (soil microbial populations and enzyme activities
viz. Urease, glucosidase, phosphatase and dehydrogenase), with organics compared to inorganic fertilizers. Compared to inorganics, there was an increase in soil organic carbon (SOC), available N, P and K by 59-65, 3-10, 10-27 and 8-25% with organics, respectively, at the end of 14
kharif years. Application of organic manures and inorganic NPK fertilizers showed marked difference on physico-chemical properties of soil (pH and EC) at tillering, panicle initiation and harvest stage of rice. At all growth stages of rice, the highest available nitrogen, phosphorus, potassium, micronutrients (Fe, Mn, Zn and Cu), urease, dehydrogenase and microbial population (bacteria, fungi and actinomycetes) in soil were recorded with application of RDNK+Dhaincha @ 10 t ha
-1.
Pattern of organic carbon (%) status from 2007 was presented in Fig 1 and the organic carbon status was medium in organic plot (0.59%) when compared to the inorganic plot (0.34%). Comparable increases in organic carbon, available N, P and K through addition of organic materials was also reported
(Carpenter-Boggs 2000 and Melero et al., 2008). Superior soil fertility status on organic farms compared to soils fertilized with chemical fertilizers was also reported by
Mader et al., 2002 and
Nataraja et al., 2021.
(Rasool et al., 2007) observed that the average mean weight diameter (MWD), total porosity and water holding capacity (WHC) were highest in FYM treated plots both in rice (0.237 mm) and wheat (0.249 mm). Application of organic manures significantly improved the soil organic carbon content and available nutrient status of soil compared to either the chemical fertilizers or the control. At the end of cropping cycle, soil organic carbon was the highest in treatment receiving vermicompost (0.69%) followed by cattle dung manure (0.68%)
(Ramesh et al., 2008).
Increased organic carbon of soil due to application of manures was reported by
(Babhulkar et al., 2000). Babu and Reddy (2000) recorded significant increase in the organic carbon content of sandy clay loam soil from 0.61 to 0.92% due to the addition of FYM and inorganic nitrogen @ 5 t ha
-1 and 50 kg ha
-1, respectively in rice.
(Hemalatha et al., 2000) reported higher content of organic carbon in soil with the application of dhaincha, followed by sunhemp and FYM.
Swarup and Yaduvanshi (2000) reported that soil organic carbon was significantly lower in treatments receiving inorganic fertilizers as compared to the treatments involving organics. According to
(Kumar et al., 2001), inclusion of green manure crop in the rice cropping system increased the organic carbon and available N, P and K of soil. Continuous and adequate use of organics with proper management can increase organic carbon content and physical properties of soils
(Atiyeh et al., 2002).
Soil physical properties like bulk density, porosity, void ratio, water permeability and hydraulic conductivity were significantly improved when FYM (10 t ha
-1) was applied in combination with chemical amendments of sodic soil
(Hussain et al., 2001). The bulk density of Vertisol decreased considerably with application of FYM (1.00 Mg m
-3) or sunnhemp incorporation (1.04 Mg m
-3) or retention of stubbles on soil surface (1.02 Mg m
-3) compared to farmer practice (1.18 Mg m
-3) is use of inorganic fertilizer
(Guled et al., 2002). Sheeba and Chellamuthu (2002) reported significant improvement in properties of VerticUstropept by continuous use of FYM @ 10 t ha
-1 over twenty two years span of time. They reported significant increase in aggregate stability (68.49%), per cent water stable aggregates (78.22) and total porosity (55.73%) with application of FYM @ 10t ha
-1 as compared to application of 100 per cent N, P
2O
5 and K
2O through inorganic fertilizers
i.e. 64.30, 75.70 and 51.03 per cent, respectively. They also noticed decrease in bulk density with the application of FYM @ 10 t ha
-1.
Grain and straw yield trends in 14 years of organic farming experiment
The pooled mean grain yield and straw yield of paddy grown in vertisols under K.C. Canal ayacut were given in Table 4. Under organic farming treatment grain yield was 4.04 t/ha while it was 5.6 t/ha under control (Inorganic/ Conventional farming) and the straw yield also was 5.07 t/ha under organic farming and 7.96 t/ha under control. The average yield increase in in organic plot was 27% and for straw it is 35%. The data on no. of tillers per hill, panicle length (cm) and no. of grains per panicle were also highest or superior in the inorganic plot compared to organic plot.
During all the 14
kharif seasons, inorganic fertilizer applied plots were near stable ranging from 6.1 to 6.8 t/ha and superior to organics (3.4 to 4.8 t/ha). This could be due to mismatch of nutrient release from organic sources and crop demand as influenced by seasonal conditions in the initial years and once the soil fertility was built up sufficiently, organic system also produced equal yields as conventional system. Thus, slow and gradual release of nutrients from organics during the initial years of conversion to organic farming could not result in increased yields. But, repeated application of organics over the years built up sufficient soil fertility by improving soil biological activity.
Grain quality parameters
Grain quality parameters recorded at the end of 2020 was presented in Table 5. Most of the grain quality parameters were not influenced even after fourten years of study, though moderate improvement in nutritional quality was recorded with organics and polishing reduced the quality improvement. Nutritional grain quality parameters-total moisture (%), total Ash (%), total Protein (%), total sugars, reducing sugars and heavy metals like chromium, cadmium and lead (Pb), pestiscide residues were not influenced by the nutrient sources even after 14 years of study. However, in the fifth year, there was an improvement in Total protein by 9.5%, with organics over inorganics (Table 5). A significant improvement in nutritional quality (Fe and Mn), with combined application of 2 or more organic sources and with 3 or 4 organic sources, Improvement in HRR, kernel length, breadth and L/B ratio after cooking with the application of organic sources alone was also reported by
Surekha and Satish Kumar 2014.