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Book of Extended summaries ISDA

Book of Extended summaries ISDA

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International Conference on Reimagining Rainfed Agro-ecosystems: Challenges &<br />

Opportunities during 22-24, December 2022 at ICAR-CRIDA, Hyderabad<br />

N3 (75% RDF as basal and 25% through fertigation) > N1 (25% RDF as basal and 75%<br />

through fertigation). Plots under N2 had 64, 11 and 18% higher DHA, APA and BGA,<br />

respectively than N1. A similar trend with lower values was observed at 15-30 cm depth.<br />

Microbial population viz., bacteria, fungi and actinomycetes was significantly affected by<br />

tillage, residue and nutrient management practices. Population <strong>of</strong> bacteria was higher<br />

compared to fungi and actinomycetes at both the soil depths though the counts were lower at<br />

(15-30) cm depth as compared to upper (0-15) cm depth. Compared to CT the counts <strong>of</strong><br />

bacteria, fungi and actinomycetes were 51, 39 and 73% higher in RT and 41, 38 and 72%<br />

higher in RR as compared to RB, respectively. The treatments having application <strong>of</strong> >50% <strong>of</strong><br />

RDF as basal (N2 and N3) had higher microbial population i.e. 40%, 60% and 70% bacteria,<br />

fungi and actinomycetes, respectively as compared to N1.<br />

Effect <strong>of</strong> tillage, residue and nutrient management on soil enzymes and microbial<br />

population<br />

Treatments<br />

Tillage (T)<br />

Dehydrogenase<br />

activity<br />

(µg TPF g -1 h -1 )<br />

Alkaline<br />

phosphatase<br />

activity<br />

(µg p-<br />

nitrophenol<br />

g -1 h -1 )<br />

ß-glucosidase<br />

activity<br />

(µg p-<br />

nitrophenol<br />

g -1 h -1 )<br />

Bacteria<br />

(CFU x 10 10<br />

g -1 soil)<br />

Fungi<br />

(CFU x<br />

10 10 g -1<br />

soil)<br />

0-15 15-30 0-15 15-30 0-15 15-30 0-15 15-30 0-15 15-<br />

30<br />

Actinomycetes<br />

(CFU x 10 10 g -1<br />

soil)<br />

0-15 15-30<br />

CT 21.67 b 17.40 b 203.64 b 197.19 b 17.14 b 16.30 b 7.93 b 6.67 b 5.69 b 4.63 b 4.43 b 3.33 b<br />

RT 91.37 a 85.76 a 276.27 a 268.06 a 26.50 a 25.63 a 11.20 a 10.06 a 7.92 a 7.66 a 7.66 a 7.48 a<br />

Residue (R)<br />

RR 43.13 b 38.61 b 227.00 b 219.45 b 20.61 b 19.73 b 7.95 b 6.78 b 5.68 b 4.64 b 4.43 b 3.41 b<br />

RB 78.79 a 73.58 a 263.50 a 255.54 a 24.98 a 24.08 a 11.19 a 10.99 a 7.83 a 7.66 a 7.61 a 7.49 a<br />

Nutrient (N)<br />

N1 41.56 c 36.69 c 226.57 c 218.86 c 20.04 b 19.12 b 7.93 b 6.86 b 5.63 b 4.59 b 4.47 b 3.43 b<br />

N2 73.24 a 68.97 a 257.26 a 249.81 a 24.61 a 23.68 a 11.17 a 10.94 a 7.87 a 7.68 a 7.59 a 7.53 a<br />

N3 68.08 b 62.63 b 251.93 b 243.82 b 23.74 a 22.91 a 11.11 a 10.86 a 7.77 a 7.69 a 7.52 a 7.39 a<br />

Different lower-case letters within same column show significant difference at P=0.05 as per<br />

Duncan Multiple Range test for mean separation<br />

Soil organic carbon content and its pools<br />

Results showed that total SOC was increased by 12 and 17% under RT and residue retention,<br />

respectively as compared CT and RB plots at 0-15 cm soil depths. In surface layer, active and<br />

passive pool carbon (6.98 and 19.45 Mg C ha-1) was 14% and 18% higher in RR plots as<br />

compared to RB, respectively after six years <strong>of</strong> continuous sugarcane cropping. Again, plots<br />

with residue retention had 63, 34 and 15% higher labile, less labile and non-labile pools,<br />

593 | Page Resource conservation and rainfed agriculture

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