Динамика влажности почвы в агрофитоценозах сои в годы, предшествовавшие засухе-2020
Закрыть
Articolul precedent
Articolul urmator
598 5
Ultima descărcare din IBN:
2023-09-21 14:54
Căutarea după subiecte
similare conform CZU
633.34:631.41:632.51 (1)
Прочие кормовые растения (119)
Почвоведение. Почвенные исследования (703)
Повреждения растений. Вредители растений. Болезни растений. Защита растений (968)
SM ISO690:2012
HARCIUC, Oleg, БАШТОВАЯ, Светлана, КИРИЛЛОВ, А.. Динамика влажности почвы в агрофитоценозах сои в годы, предшествовавшие засухе-2020. In: Protecţia plantelor - realizări şi perspective, Ed. 57, 27-28 octombrie 2020, Кишинев. Кишинев: "Print-Caro" SRL, 2020, nr.57, pp. 355-359. ISBN 978-9975-3472-0-4. DOI: https://doi.org/10.53040/9789975347204.85
EXPORT metadate:
Google Scholar
Crossref
CERIF

DataCite
Dublin Core
Protecţia plantelor - realizări şi perspective
nr.57, 2020
Simpozionul "Protecţia plantelor - realizări şi perspective"
57, Кишинев, Moldova, 27-28 octombrie 2020

Динамика влажности почвы в агрофитоценозах сои в годы, предшествовавшие засухе-2020

DOI: https://doi.org/10.53040/9789975347204.85
CZU: 633.34:631.41:632.51

Pag. 355-359

Harciuc Oleg, Баштовая Светлана, Кириллов А.
 
Институт генетики, физиологии и защиты растений
 
Disponibil în IBN: 28 octombrie 2020


Rezumat

In the soybean cenosis (mainly the Aura variety) with a characteristic density (400-500 × 103 plants/ha), the dynamics of soil moisture in the years preceding the drought-2020 was studied. The main factor of drought-2020 is the low (about 100 mm lower than the average annual value) moisture accumulation in the soil before sowing for the autumn-spring 2019/2020, mainly due to low precipitation. An additional prerequisite for drought-2020 is a decrease in soil moisture (including deep soil layers) during harvesting in recent years, which is the reason for an additional deficit in a soil layer 0-100 cm of approximately 25 mm of water.

Cuvinte-cheie
Soybean, Soil moisture, Drought, cenosis

DataCite XML Export

<?xml version='1.0' encoding='utf-8'?>
<resource xmlns:xsi='http://www.w3.org/2001/XMLSchema-instance' xmlns='http://datacite.org/schema/kernel-3' xsi:schemaLocation='http://datacite.org/schema/kernel-3 http://schema.datacite.org/meta/kernel-3/metadata.xsd'>
<creators>
<creator>
<creatorName>Harciuc, O.A.</creatorName>
<affiliation>Institutul de Genetică, Fiziologie şi Protecţie a Plantelor, Moldova, Republica</affiliation>
</creator>
<creator>
<creatorName>Baştovaia, S.I.</creatorName>
<affiliation>Institutul de Genetică, Fiziologie şi Protecţie a Plantelor, Moldova, Republica</affiliation>
</creator>
<creator>
<creatorName>Kirillov, A.</creatorName>
<affiliation>Institutul de Genetică, Fiziologie şi Protecţie a Plantelor, Moldova, Republica</affiliation>
</creator>
</creators>
<titles>
<title xml:lang='ru'>Динамика влажности почвы в агрофитоценозах сои в годы, предшествовавшие засухе-2020</title>
</titles>
<publisher>Instrumentul Bibliometric National</publisher>
<publicationYear>2020</publicationYear>
<relatedIdentifier relatedIdentifierType='ISBN' relationType='IsPartOf'>978-9975-3472-0-4</relatedIdentifier>
<subjects>
<subject>Soybean</subject>
<subject>Soil moisture</subject>
<subject>Drought</subject>
<subject>cenosis</subject>
<subject schemeURI='http://udcdata.info/' subjectScheme='UDC'>633.34:631.41:632.51</subject>
</subjects>
<dates>
<date dateType='Issued'>2020</date>
</dates>
<resourceType resourceTypeGeneral='Text'>Conference Paper</resourceType>
<descriptions>
<description xml:lang='en' descriptionType='Abstract'><p>In the soybean cenosis (mainly the Aura variety) with a characteristic density (400-500 &times; 103 plants/ha), the dynamics of soil moisture in the years preceding the drought-2020 was studied. The main factor of drought-2020 is the low (about 100 mm lower than the average annual value) moisture accumulation in the soil before sowing for the autumn-spring 2019/2020, mainly due to low precipitation. An additional prerequisite for drought-2020 is a decrease in soil moisture (including deep soil layers) during harvesting in recent years, which is the reason for an additional deficit in a soil layer 0-100 cm of approximately 25 mm of water.</p></description>
</descriptions>
<formats>
<format>application/pdf</format>
</formats>
</resource>