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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 />

and soil loss over the future periods was estimated using the respective baseline values.<br />

Plausible adaptation strategies were simulated in two categories: (i) residue<br />

addition/mulching (organic and inorganic) and (ii) sub-surface drainage system (plastic pipes<br />

and clay tile at 0.61 m deep) on cultivated HMWs, i.e., HMW3 to HMW6. The residue<br />

considered to be locally available dry beans, field beans, soybeans, maize, broom grasses, and<br />

stone mulch in the inter-cropped area.<br />

Results<br />

Measured soil erosion revealed that forests (HMW 1) had a mean (<strong>of</strong> 24 years) annual run<strong>of</strong>f<br />

loss <strong>of</strong> 405.5 (±113) mm, while soil loss was 11.0 (±2.4) Mg ha -1 yr -1 . In the cultivated<br />

HMWs (HMW4, 5 & 6), adoption <strong>of</strong> soil water conservation measures (SWCMs) reduced the<br />

run<strong>of</strong>f by 13.0% – 17.1% and soil loss by 12.6%–15.1% over HMW 1. However, in shifting<br />

cultivation (HMW7), run<strong>of</strong>f increased by 50.6%–87.6%, while soil loss was 50.3%–59.8%<br />

higher over the forest. The average annual run<strong>of</strong>f calibrated and validated by the<br />

WEPP model was comparable to the measured run<strong>of</strong>f and the differences were negligible (p<br />

< 0.05). The normalized RMSEn was 0.81<br />

during calibration and >0.75 during validation periods for all HMWs, indicating that model<br />

performance could be assessed as "very good".<br />

The projected annual SE (average) for all HMWs increased in all RCPs. The IFS based on<br />

shifting cultivation (HMW2) was the most vulnerable, with the highest percentage increase in<br />

SE (46–235%) compared to the baseline years under RCP 8.5. The cultivated IFSs (HMW3 to<br />

HMW 6) had 47.8–57.0% less run<strong>of</strong>f and 39.2–74.6% less soil loss than HMW 2 under RCP<br />

8.5. Of these, HMW6 followed by HMW4 and HMW5 were more effective in minimizing soil<br />

loss (Table 1). The simulated the effects <strong>of</strong> mulching (both organic and inorganic) in all the<br />

cultivated IFSs (HMW 3 to HMW 6) declined with an increase in the mulch application rate<br />

from 5.0 to 20 t ha -1 . Among organic mulches used, broom grass mulching at an application<br />

rate <strong>of</strong> 20 t ha -1 resulted in a maximum reduction in soil loss <strong>of</strong> 8.7, 9.3, and 11.9 t ha -1 yr -1 in<br />

the years 2020s, 2050s, and 2080s, respectively, compared to non-mulching. However, with a<br />

low residue application <strong>of</strong> 5 t ha -1 , dry bean residues were most effective in controlling soil<br />

erosion. Under stone mulching, simulated soil loss is projected to decrease in the range <strong>of</strong> 7.7<br />

to 13.3 t ha -1 yr -1 when applied @ 20 t ha -1 during 2080s. The adoption <strong>of</strong> underground<br />

drainage systems has demonstrated that the 6-inch diameter plastic pipe installed at a distance<br />

<strong>of</strong> 7 m provides a greater reduction in projected SE than a clay tile <strong>of</strong> the same diameter<br />

installed at a distance <strong>of</strong> 24 meters.<br />

Climate resilient agriculture for risk mitigation<br />

291 | Page

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