Soil compaction is a well-known thr

Soil compaction is a well-known threat to soil quality. Numerous studies have highlighted the effects of this phenomenon, which involve different consequences for physical, chemical and biological processes in the soil profile (Berisso et al., 2013; Beylich et al., 2010; Thomas et al., 2019; Weisskopf et al., 2010). Compaction in the soil occurs when an external force or stress is larger than the internal soil strength, which is dependent on texture, matric potential and soil aggregation. If the stresses exceed the soil strength, the result will be plastic deformation (Horn et al., 1995). When soil compaction occurs, properties like bulk density, aggregate size, infiltration rates, and soil strength change considerably. These changes can be detrimental to soil quality, affecting multiple soil functions, decreasing production yields and increasing the risk of soil erosion (Soane and van Ouwerkerk, 1995).

Результаты (узбекский) 1:

Tuproqning siqilishi tuproq sifatiga mashhur tahdiddir. Ko'pgina tadqiqotlar tuproq profilidagi fizik, kimyoviy va biologik jarayonlar uchun turli xil oqibatlarni o'z ichiga olgan ushbu hodisaning ta'sirini ta'kidladi (Berisso va boshq., 2013; Beylich va boshq., 2010; Tomas va boshq., 2019; Weisskopf va boshqalar. ., 2010). Tuproqdagi siqilish tashqi kuch yoki kuchlanish tuproqning ichki kuchidan kattaroq bo'lganda sodir bo'ladi, bu teksturaga, matrik potensialga va tuproq agregatsiyasiga bog'liq. Agar kuchlanishlar tuproqning mustahkamligidan oshsa, natijada plastik deformatsiya bo'ladi (Horn va boshqalar, 1995). Tuproqning siqilishi sodir bo'lganda, massa zichligi, agregat hajmi, infiltratsiya tezligi va tuproq kuchi kabi xususiyatlar sezilarli darajada o'zgaradi. Bu o'zgarishlar tuproq sifatiga salbiy ta'sir ko'rsatishi, tuproqning ko'plab funktsiyalariga ta'sir qilishi, hosildorlikning pasayishi va tuproq eroziyasi xavfini oshirishi mumkin (Soane va van Ouwerkerk, 1995).