Effect of various land configurations on soil charactersics, nutrient loss and peak discharge of stage hydrograph

M. P. Sathe, M. Kale, S. Lad
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Abstract

In order to study the various land configurations and the impact of soil and water conservation measures in terms of improving the in soil characterstics, soil nutrients and reduction in soil and nutrient losses, three land configurations were studied for soil-water management, viz., cultivation along the slope with opening of tide furrow (T 1 ), contour cultivation with opening of alternate furrow (T 2 ) and contour cultivation with opening of ridges and furrows (T 3 ). The present investigation revealed that the treatment T 3 was more prominent and favourably influenced the soil characterstics, soil nutriestsdue to the drastic change in the runoff hydrograph characteristics and reduction soil loss and nutrient losses, followed by treatment T 2 over the treatment T 1 . In the context of above results, it is concluded that the various land configurations measures is the need of day in rainfed agriculture for the management of erratic and vagarious rainfall and improving the in soil characterstics and soil nutrients under the changing climatic conditions. The runoff occurred in all the treatments were due to second storm only. While comparing the peak discharge among all the treatment, it was found that, the treatment T 1 had highest peak discharge 11.7 lps followed by treatment T 2 (10.7 lps) and treatment T 3 (2.03 lps). It was found that in treatment T 2 nitrogen (N) loss reduced from 21.82 kg ha to 2.4kg ha (i.e.89.00 %) over the treatment T 1 and in treatment T 3 it was reduced upto 0.59 kg ha (i.e. 95.46%) over T 1 .There was same trend was observed in case of phosphorus (P) and potassium (K).
不同土地形态对土壤特征、养分流失和阶段水文峰值流量的影响
为了研究各种土地配置和水土保持措施的影响而言,改善土壤特点,减少土壤养分和土壤和养分损失,三个土地配置水保管理进行了研究,即,沿着山坡种植与开放潮沟(T 1)等高线种植与开放替代沟(T 2)和等高线种植的山脊和沟(T 3)。结果表明,由于径流水文特征的显著变化和土壤流失量和养分损失的减少,处理t3对土壤特征和土壤养分的影响更为显著,其次是处理t2,而不是处理t1。综上所述,在气候条件不断变化的条件下,多种土地配置措施是旱作农业管理不稳定和不稳定降雨、改善土壤特性和土壤养分的需要。所有处理的径流都是由第二次暴雨引起的。在比较各处理的峰值流量时,发现t1处理的峰值流量最高,为11.7 lps,其次是t2处理(10.7 lps)和t3处理(2.03 lps)。结果表明,与t1相比,t2处理氮(N)损失从21.82 kg hm2减少到2.4kg hm2 (89.00%), t3处理氮(N)损失比t1减少到0.59 kg hm2(95.46%),磷(P)和钾(K)也有相同的趋势。
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