EI·Kot, A., EI-Eweddy, E. (2002). SOIL PHYSICAL AND CHEMICAL PROPERTIES AS INFLUENSED BY DRAINAGE AND TILLAGE IN ELSA LAM CANAL AREA.. Journal of Soil Sciences and Agricultural Engineering, 27(8), 5679-5691. doi: 10.21608/jssae.2002.255227
A.S. EI·Kot; E.A. EI-Eweddy. "SOIL PHYSICAL AND CHEMICAL PROPERTIES AS INFLUENSED BY DRAINAGE AND TILLAGE IN ELSA LAM CANAL AREA.". Journal of Soil Sciences and Agricultural Engineering, 27, 8, 2002, 5679-5691. doi: 10.21608/jssae.2002.255227
EI·Kot, A., EI-Eweddy, E. (2002). 'SOIL PHYSICAL AND CHEMICAL PROPERTIES AS INFLUENSED BY DRAINAGE AND TILLAGE IN ELSA LAM CANAL AREA.', Journal of Soil Sciences and Agricultural Engineering, 27(8), pp. 5679-5691. doi: 10.21608/jssae.2002.255227
EI·Kot, A., EI-Eweddy, E. SOIL PHYSICAL AND CHEMICAL PROPERTIES AS INFLUENSED BY DRAINAGE AND TILLAGE IN ELSA LAM CANAL AREA.. Journal of Soil Sciences and Agricultural Engineering, 2002; 27(8): 5679-5691. doi: 10.21608/jssae.2002.255227
SOIL PHYSICAL AND CHEMICAL PROPERTIES AS INFLUENSED BY DRAINAGE AND TILLAGE IN ELSA LAM CANAL AREA.
Soli Conservation Dept, Desert Research Center, Calro,Egypt
Abstract
A field study was conducted in heavy clay salt affected soil at 83km along EI- Salam canal (North plain Husseiniya) to evaluate suitability open drainage system with 30-m space between the drains with two tillage depths 15 and 25-cm for improving some physical and chemical properties of soil and to improve its productivity. The data were collected through two growing season (Berseem, winter of 200012001 and Corn summer of 2001). Soil contents of total and available N.P.K. and some chemical properties (EC, pH, SAR and ESP) were studies. The soil samples were taken from four sites between the drains and the distances 10-m between all samples along the mid- way at depths 0-15,15-30,30-60 and S0-9Ocm. The obtained results showed that, the content of soluble salts EC, pH, SAR and ESP increased with the increase of soil depth and decreased with the increase of tillage depths. Also this decrease was clear in the surface layers compared with the decrease occurred in the down layers. Data show that, both total and available N, P and K decreased with increasing soil depth before and after drained and tillage treatment. This decreased In the N.P.K. values was more clear in the soil profile with drained and tillage depth 25-crn than with tillage depth 15-cm. This decreased may by due to the low content of organic malter and high soli pH values In the lower layers of soil profiles. The high loss of available N and P resulted from down movement of available and organiC matter with leaching water. Data also show that, the available (N) increase with tillage treatments. The calculated relative increases of N. were 7.4 and 20 % with tillage depth 25 and 15-cm of the soil " before tillage and drained. While, the values of the available (P and K) decrease with tillage treatments, the relative decrease of (P and K) were 18.9 and22.3 %, 71.9 and 52.5% in the soil profile with drained and tillage depth 25-cm and 15-cm.
The bulk density of the deeper layers is relatively higher than those of the upper ones. The lowest bulk density is obtained in the solis provided with open drainage and tillage depth 25-cm. With respect to the porosity, it was found out that, the total porosity (E %) Increases with decreasing of the bulk density. The open drainage system with tillage deep 25-cm is more efficient in Increasing soil hydraulic conductivity comparing with the other process. Also, hydraulic conductivity increased with Increasing electrolyte concentration but decreased with increasing SAR. The lowering of CaC03 % content under open drained and tillage conditions may by due to the high leaching and movement efficiency than before drained and tillage. The organic matter's content decreases with increasing soil depth and tillage depth. The drainage condition appears no effect on texture class because this soil parameter is considered as initial, but the tillage operation one of the most treatments to be changed. The regression equations and correlation coefficients (r) between the hydraulic conductivity and each of EC, CaC03, clay, ESP and ASR. Also, between the vavailable content of N, P and K and each of EC, ASR, and ESP were computed. Results , also show that the yields obtained from the soil provided by
drainage and tillage are higher than those obtained from the non- drained and tillage soils.
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