Effects of water-saving pruning on the growth and water consumption of jujube (Ziziphus jujuba Mill.) in a loess hilly region with deep soil desiccation

Jianpeng Ma,Xing Wang,Youke Wang,Wenfei Zhang,Xining Zhao

doi:10.2166/ws.2021.117

Abstract

Abstract In order to study whether jujube trees can grow normally under rain-fed conditions in loess hilly areas, we planted jujube trees (Ziziphus jujuba Mill.) 4 years after felling a 23-year-old apple orchard. The growth process of the jujube trees and the variation in soil water content (SWC) were monitored for three consecutive years following planting in order to study the effects of the water-saving pruning (WSP) technique. Results showed the following. (1) The soil at a depth of 0–1,000 cm had been desiccated when the area was an apple orchard. (2) Under rain-fed conditions, the jujube trees with the WSP technique were always able to maintain normal growth while the jujube trees with conventional pruning method had a normal growth stage of only 4 years. The water use efficiency of the jujube trees with the WSP technique was much higher than that of the jujube trees with conventional pruning. We recommend WSP in jujube orchard management, because the jujube trees with WSP could maintain normal growth in the deep dried soils of the loess hilly region, as WSP can reduce the water consumption of the jujube trees and may have a positive effect on soil moisture restoration.

Highlights

In the loess region of China, groundwater is deeply buried, meaning that the main source soil water is precipitation
(2) Under rain-fed conditions, the jujube trees with the water-saving pruning (WSP) technique were always able to maintain normal growth while the jujube trees with conventional pruning method had a normal growth stage of only 4 years
We proposed water-saving pruning for the growth of jujube trees planted in dry soil

Summary

Introduction

In the loess region of China, groundwater is deeply buried, meaning that the main source soil water is precipitation. The depth of infiltration is usually less than 200 cm in loess regions without deep leakage. Once these dried layers appeared, they did not return to normal even after many years, they could be called permanently dried layers (Wang et al ). Present studies show that the depth of soil moisture depletion in perennial planted vegetation can reach up to 1,000 cm

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