Degradation and restoration of soil structure in a cracking grey clay used for cotton production

Soil Research ◽  
1989 ◽  
Vol 27 (2) ◽  
pp. 455 ◽  
Author(s):  
IG Daniells

A field experiment involving irrigated cotton investigated the effect of tillage on a self-mulching cracking grey clay at three different soil water contents: dry (close to permanent wilting point to over 1 m depth), moist (subsoil close to the lower plastic limit) and wet (just trafficable). These treatments had been repeated over three years prior to the plant and soil measurements reported in this paper. Compared with tillage of dry soil, tillage of moist or wet soil depressed lint yield by 35% (P<0.001). Shrinkage curves of resin-coated, intact soil clods showed lower clod bulk density at a standard water content in the dry treatment than in the wet treatment (P<0.001). This difference was most marked in the 0.2-0.3 m depth, where clods from the wet treatment had a bulk density approaching that of clods made from hand-remoulded soil. Subsequent restoration treatments showed that, although wheat improved soil physical condition, the yield of a following cotton crop was reduced due to lower nitrogen uptake (P<0.001). Deep tillage alone increased clod bulk density but deep tillage after wheat decreased density (interaction P<0.001 for the 0.2-0.3 m depth, P<0.05 for the 0.3-0.4 m depth). These effects of deep tillage were not reflected in yield of cotton. Effects of the previous dry, moist and wet tillage treatments persisted but there was some improvement, even in the absence of restoration treatments. To preserve the structure and productivity of cracking clay soils, they should be tilled only when dry to permanent wilting point through the full depth of tillage.


2020 ◽  
Vol 16 (No. 1) ◽  
pp. 29-38
Author(s):  
Jan Vopravil ◽  
Pavel Formánek ◽  
Tomáš Khel

Soil properties can be influenced by long-term agricultural management practices as described in pedological literature. In this study, selected physical properties (particle density and bulk density, total porosity, maximum capillary water capacity, minimum air capacity, field capacity, permanent wilting point and available water capacity) of topsoils from different reference soil groups (Cambisols, Luvisols, Fluvisols, Chernozems and Phaeozems, Leptosols, Stagnosols and Gleysols) were sampled and analysed in the years 2016–2017. The topsoil samples were taken from points of so-called S (specific) soil pits to be sampled from the General Soil Survey of Agricultural Soils (GSSAS) which was accomplished in the years 1961–1970. In addition, some of the properties were also compared with those measured during the GSSAS. Recognising the properties, only the particle density, the maximum capillary water capacity, the permanent wilting point and the available water capacity of the topsoil of the individual soil groups were statistically significantly (P &lt; 0.05) different. A comparison of the physical properties with those analysed after more than 40 years was performed, the bulk density increased and the total porosity decreased in the topsoil of the major part of the studied soil groups.



2018 ◽  
Vol 64 (9) ◽  
pp. 1240-1253 ◽  
Author(s):  
Tülay Tunçay ◽  
Oğuz Başkan ◽  
Ilhami Bayramın ◽  
Orhan Dengız ◽  
Şeref Kılıç


2018 ◽  
pp. 6-17
Author(s):  
І. Prymak ◽  
А. Panchenko ◽  
M. Voitovyk ◽  
V. Karpenko ◽  
S. Levandovska ◽  
...  

The evolutional way of developing of the theoretical and practical basis of main tillage since the middle of the first part of the 20th century up today is highlighted. Exaggerated ideologization of science, government monopoly of academician V.R. Williams from thirties to fifties years of the 20th century caused big losses in agrarian science, especially in farming and agriculture sciences. The disaster of Williams was caused by absolute priority of soil conditioning and universalization of developed by him grass rotation system of farming. Till fifties in crop farming arable tillage to the depth at least 20–22 cm dominated completely. The first person in the USSR to refuse from a plough was T.S. Maltsev who recommended to hold deep beardless tillage once in 4–5 years, and for the rest of the time to use surface one (up to 8 cm) or surface tillage (10–12 cm) with discs. After T.S. Maltsev works, the issues of differentiation of tilled soil layers under beardless and surface tillage became especially controversial. The final boost for the development of theoretical and practical basis of tillage minimization was soil protecting system suggested by the group of scientists of the former All-Soviet Union Research Institute of grain growing headed by O.І. Baraievyi. It was based on beardless tillage, sowing with stubbly seeding machines, flap and buffer planting, snow capture etc. Early adopters of a full refusal from beard tillage in Ukraine during 80–90ies years were І.Ye. Shcherbak, F.M. Morgun, M.K. Shykula, S.S. Antonets and their students and followers. Nowadays the majority of national scientists consider the differential different depth tillage as the most effective one during crop rotations, which includes alternation of different ways, events and means of soil tillage depending on ecological conditions, crops biological features, structure of crop acreage, fertilization systems and plants protection etc. In scientists opinion, the minimal tillage is available on 3 millions of hectare and no-tillage is available on 5,49 millions of hectare out of 30 millions of tilled soils in Ukraine. In thirties V.R. Williams and M.S. Sokolov criticized surface tillage. Academician M.M. Tulaykov who was openly against doctrines of V.R. Williams recommended surface tillage in dry regions which in his opinion had to protect tilled soil from wind formed processes. He claimed that surface tillage is economically suitable for poor husbandries and that dust storms are the result of a constant daily soil drifting caused by deep tillage. In forties an American farmer E. Folkner widely promoted surface tillage together with soil mulching with plant matters of green crops. The first person to refuse from beard tillage in the first part of the 20th century in the Soviet empire was T.S. Maltsev. He proved decisively the advantages of beardless tillage over beard one in Transurals. T.S. Maltsev suggested the whole range of tools for soil tillage developed by him, the main of which were cultrate pulverizers and a beardless plough. The necessity of tillage with plough was the main stereotype existing in the world tillage theory and practice till the fifties. Scientific inheritance of M.M. Tulaykov became one of the bases for reconsideration of the concept of V.R. Williams existing in Ukraine. He concluded that it was necessary to change beard tillage to surface one to the depth 10-12 cm under which root system of one-year-old plants would be decomposed in tight soil where anoxic conditions must dominate. And to cultivate bottom layers it was necessary to hold deep tillage with beardless ploughs once in 4–5 years. The first person to refuse from a plough in the USSR was T.S. Maltsev. He suggested using surface plowing with disc tillers and deep beardless tillage (40–50 cm) once in 4–5 years instead of tillage in crops rotation of Transural. In 1952 he made a beardless plough for the first time. The most controversial issue among the scientists of Ukraine was differentiation of the tilled layer and its effect on crop productivity under beardless and surface tillage. In sixties and seventies O.I. Baraiev and his colleagues from All Soviet Union Research Institute of grain farming headed by him developed for the first time a soil protective system based exceptionally on different depth beardless tillage in crop rotations, usage of stubbly seeding machines, subsurface cultivators, soil spikers, coulisse fallow, buffer planting etc. In Ukraine during eighties and nineties years a complete refusal from beard tillage in favor of beardless tillage was supported by І.Ye. Shcherbak, F.T. Morgun, M.K. Shykula, S.S. Antonets and other scientists and experts. High weed infestation of fields under such tillage was the main obstacle to its widespread usage. In the 21st century the majority of scientists recommend differential different depth main tillage which suggests different ways, events and means of its implementation in crop rotations depending on biological features of crop, soil and climate conditions, fertilizing systems, plant protection etc, 13 millions hectare of tilled soil is technologically suitable for minimum tillage in Ukraine, and the rest 5,5 million hectare do not even need tillage at all. Key words: tillage, soil, evolution, plough, subsurface cultivator, erosion, minimization, differentiation.



1984 ◽  
Vol 21 (1-2) ◽  
pp. 109-124 ◽  
Author(s):  
R.H. Sauer ◽  
M.L. Warner ◽  
W.T. Hinds


2019 ◽  
Vol 71 (3) ◽  
pp. 392-398 ◽  
Author(s):  
Chong Chen ◽  
Hu Zhou ◽  
Jianying Shang ◽  
Kelin Hu ◽  
Tusheng Ren


Geosciences ◽  
2020 ◽  
Vol 10 (4) ◽  
pp. 117 ◽  
Author(s):  
Ahmed Abed Gatea Alshammary ◽  
Abbas Z. Kouzani ◽  
Akif Kaynak ◽  
Sui Yang Khoo ◽  
Michael Norton ◽  
...  

The estimation of soil wet bulk density (ρn) and dry bulk density (ρb) using the novel digital electromechanical system (DES) has provided information about important parameters for the assessment of soil quality and health with a direct application for agronomists. The evaluation of the DES performance is particularly appropriate for different tillage methods, mulching systems, and fertilizers used to increase soil fertility and productivity, but currently, there is a lack of information, particularly in the arid areas in underdeveloped countries. Therefore, the main aim of this study was the application of a novel digital electromechanical system (DES) to evaluate bulk density, wet (ρn) and dry (ρb), under different soil treatments according to the variations in thermal efficiencies (ηth), microwave penetration depths (MDP), and specific energy consumption (Qcon) in an experimental area close to Baghdad (Iraq). The experimental design consisted of 72 plots, each 4 m2. The agronomic practices included two different tillage systems (disc plough followed by a spring disk and mouldboard plough followed by a spring disk) and twelve treatments involving mulching plastic sheeting combined with fertilizers, to determine their effect on the measured soil ρn and ρb and the DES performance in different soils. The results indicated that soil ρn and ρb varied significantly with both the tillage systems and the mulching systems. As expected, the soil ρn and ρb, MDP, and Qcon increased with an increase in the soil depth. Moreover, the tillage, soil mulching, and soil depth value significantly affected ηth and Qcon. A strong relationship was identified between the soil tillage and MDP for different soil treatments, leading to the changes in soil ρb and the soil dielectric constant (ε’).





2011 ◽  
Vol 57 (2) ◽  
pp. 45-52
Author(s):  
Dana Kotorová ◽  
Jana Jakubová ◽  
Ladislav Kováč

Dependence of Heavy Soil Transport Function on Soil Profile DepthThe aim of this work was to quantify the effect of soil profile depth on the transport function of heavy soils. Treatments were carried out between 2006 and 2009 in Milhostov. Two variants were examined : the (conventional soil tillage and long-time no-tilled variant). Soil samples were taken in spring and autumn from soil profile depth of 0.00-0.60 m from each 0.10 m. For further evaluation the average values were used. Particle size composition, bulk density, total porosity and maximum capillary capacity were determined. Content of clay particles in soil profile was in interval 59.64-68.53% and such soils are characterised in the range from clay-loamy soil to clayey soil. The bulk density increased with the depth of soil profile and its values reached 1 184-1 646 kg m-3. The total porosity was in range 37.68-55.17% and it decreased with the depth of soil profile. The values of maximum capillary capacity were characterised for heavy soils with high content of clay particles. The depth had statistically significant effect on all observed parameters. In average, on both variants the bulk density was higher than 1 400 kg m-3, the total porosity was lower than 47% and the content of clay was higher than 30%, pointing to the possibility of soil compaction, which will result in reduced transport function of heavy soils.



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