Zobrazeno 1 - 10
of 902
pro vyhledávání: '"H. Emami"'
Publikováno v:
مجله آب و خاک, Vol 37, Iss 3, Pp 415-430 (2023)
Introduction Changes in soil properties depend on factors such as climate, topography, landscape features, altitude, parent material, and vegetation. The quantity and quality of soils obtained from different rocks (igneous, sedimentary and metamorphi
Externí odkaz:
https://doaj.org/article/ca4b7845839f413fb492269421065635
Publikováno v:
Majallah-i ̒Ulum-i Bāghbānī, Vol 37, Iss 2, Pp 541-560 (2023)
IntroductionChromium pollution of the soil due to natural processes or industrial activities such as metal refining, chrome plating, stainless-steel production, leather tanning, and chemical dye production is a globle environmental issue. Excessive s
Externí odkaz:
https://doaj.org/article/a824715148694c238e4536f7ec1ac2c4
Autor:
H. Emami, M. Memarzadeh
Publikováno v:
مجله آب و خاک, Vol 37, Iss 2, Pp 219-235 (2023)
Introduction Wind Erosion is the natural process of transportation and deposition of soil by wind. It is a common phenomenon occurred mostly in dry, sandy soils or anywhere the soil is loose, dry, and finely granulated. Heavy metals are found in the
Externí odkaz:
https://doaj.org/article/6834e0c3cc62430f9c01c42062c90a6c
Publikováno v:
مجله آب و خاک, Vol 36, Iss 1, Pp 95-112 (2022)
Introduction The type of management operations and land use systems are the key parameters affecting the soil quality and sustainable land use. The exploitation systems by efficient use of soil and water recourse can decrease productions costs and in
Externí odkaz:
https://doaj.org/article/43137691c4a043a2a0d59aae34fb048e
Publikováno v:
مجله آب و خاک, Vol 36, Iss 1, Pp 113-126 (2022)
IntroductionSoil salinity has a negative effect on physical, chemical and biological properties of soil. Salinity also affects the relationships between soil and plants, which in turn has a significant effect on plant growth. One of the solutions use
Externí odkaz:
https://doaj.org/article/edb1880bd94b4c78b9b63ddbff3f1e9e
Autor:
M. Rahmati, L. Weihermüller, J. Vanderborght, Y. A. Pachepsky, L. Mao, S. H. Sadeghi, N. Moosavi, H. Kheirfam, C. Montzka, K. Van Looy, B. Toth, Z. Hazbavi, W. Al Yamani, A. A. Albalasmeh, M. Z. Alghzawi, R. Angulo-Jaramillo, A. C. D. Antonino, G. Arampatzis, R. A. Armindo, H. Asadi, Y. Bamutaze, J. Batlle-Aguilar, B. Béchet, F. Becker, G. Blöschl, K. Bohne, I. Braud, C. Castellano, A. Cerdà, M. Chalhoub, R. Cichota, M. Císlerová, B. Clothier, Y. Coquet, W. Cornelis, C. Corradini, A. P. Coutinho, M. B. de Oliveira, J. R. de Macedo, M. F. Durães, H. Emami, I. Eskandari, A. Farajnia, A. Flammini, N. Fodor, M. Gharaibeh, M. H. Ghavimipanah, T. A. Ghezzehei, S. Giertz, E. G. Hatzigiannakis, R. Horn, J. J. Jiménez, D. Jacques, S. D. Keesstra, H. Kelishadi, M. Kiani-Harchegani, M. Kouselou, M. Kumar Jha, L. Lassabatere, X. Li, M. A. Liebig, L. Lichner, M. V. López, D. Machiwal, D. Mallants, M. S. Mallmann, J. D. de Oliveira Marques, M. R. Marshall, J. Mertens, F. Meunier, M. H. Mohammadi, B. P. Mohanty, M. Pulido-Moncada, S. Montenegro, R. Morbidelli, D. Moret-Fernández, A. A. Moosavi, M. R. Mosaddeghi, S. B. Mousavi, H. Mozaffari, K. Nabiollahi, M. R. Neyshabouri, M. V. Ottoni, T. B. Ottoni Filho, M. R. Pahlavan-Rad, A. Panagopoulos, S. Peth, P.-E. Peyneau, T. Picciafuoco, J. Poesen, M. Pulido, D. J. Reinert, S. Reinsch, M. Rezaei, F. P. Roberts, D. Robinson, J. Rodrigo-Comino, O. C. Rotunno Filho, T. Saito, H. Suganuma, C. Saltalippi, R. Sándor, B. Schütt, M. Seeger, N. Sepehrnia, E. Sharifi Moghaddam, M. Shukla, S. Shutaro, R. Sorando, A. A. Stanley, P. Strauss, Z. Su, R. Taghizadeh-Mehrjardi, E. Taguas, W. G. Teixeira, A. R. Vaezi, M. Vafakhah, T. Vogel, I. Vogeler, J. Votrubova, S. Werner, T. Winarski, D. Yilmaz, M. H. Young, S. Zacharias, Y. Zeng, Y. Zhao, H. Zhao, H. Vereecken
Publikováno v:
Earth System Science Data, Vol 10, Pp 1237-1263 (2018)
In this paper, we present and analyze a novel global database of soil infiltration measurements, the Soil Water Infiltration Global (SWIG) database. In total, 5023 infiltration curves were collected across all continents in the SWIG database. Thes
Externí odkaz:
https://doaj.org/article/9f4b28dc6d4740a49331b641f176445f
Publikováno v:
مجله آب و خاک, Vol 30, Iss 6, Pp 2060-2077 (2017)
Introduction: Gully erosion is an important type of soil erosion in Iran and Ardebil province (Moghimi and Salami, 2011; Khatibi, 2006). Increasing the cross section of gullies is an indicator for gully developing (Deng et al, 2015). Topography and s
Externí odkaz:
https://doaj.org/article/a05cbf82e67748a4964530494976d6f9
Publikováno v:
مجله آب و خاک, Vol 29, Iss 5, Pp 1333-1344 (2017)
Introduction: Soil erosion by water is one of the most widespread forms of land degradation and it has caused many undesirable consequences in last decades. On steep slopes, rill erosion is the most important type of erosion, which produces sediment
Externí odkaz:
https://doaj.org/article/4d01679aa7e545d3b68288a1a3dd0dfa
Publikováno v:
مجله آب و خاک, Vol 29, Iss 6, Pp 1699-1710 (2016)
Introduction: Topography is an important and effective property affecting the soil quality. Some researchers demonstrated that degree and aspect of land slope may influence the particle size distribution and gravel. Slope degree affects the surface a
Externí odkaz:
https://doaj.org/article/bc26d1a1b9f84584a52f8530db0e01dd
Publikováno v:
مجله آب و خاک, Vol 29, Iss 3, Pp 673-682 (2016)
Introduction: Saffron is one of the most important economic plants in the Khorasan province. Awareness of soil quality in agricultural lands is essential for the best management of lands and for obtaining maximum economic benefit. In general, plant g
Externí odkaz:
https://doaj.org/article/ede113a194484a23817564e9a7fea4b3